Sample records for temperature cdiac climate

  1. Climate Data from the Carbon Dioxide Information Analysis Center (CDIAC)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    CDIAC products are indexed and searchable through a customized interface powered by ORNL's Mercury search engine. Products include numeric data packages, publications, trend data, atlases, models, etc. and can be searched for by subject area, keywords, authors, product numbers, time periods, collection sites, spatial references, etc. Some of the collections may also be included in the CDIAC publication Trends Online: A Compendium of Global Change Data. Most data sets, many with numerous data files, are free to download from CDIAC's ftp area. CDIAC lists the following collections under the broad heading of climate information: Global Temperature, Precipitation, Sea Level Pressure, and Station Pressure Data, United States Temperature, Precipitation, and Snow Data, USSR and People's Republic of China Climate Data, Cloud and Sunshine Data, and Other Climatic Data.

  2. Carbon Dioxide Information Analysis Center (CDIAC) PRINCIPAL INVESTIGATOR: Thomas A Boden (CDIAC Di-

    E-Print Network [OSTI]

    Carbon Dioxide Information Analysis Center (CDIAC) PRINCIPAL INVESTIGATOR: Thomas A Boden (CDIAC Di of Biological and Environmental Research (BER) PARTNERS: National Aeronautic and Space Administra- tion's (NASA://cdiac.ornl.gov/ PROJECT DESCRIPTION The Carbon Dioxide Information Analysis Center (CDIAC) is the primary climate -change

  3. ORNL/CDIAC-159 PACIFICA DATA SYNTHESIS PROJECT

    E-Print Network [OSTI]

    2013 Prepared for the Climate Change Research Division Office of Biological and Environmental Research & Carbon Hydrographic Data Office CDIAC Carbon Dioxide Information Analysis Center CFCs Chlorofluorocarbons University, USA 7 Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, US DOE, USA 8

  4. ORNL/CDIAC-147 DOI: 10.3334/CDIAC/atg.ndp001.2004

    E-Print Network [OSTI]

    of Biological and Environmental Research U.S. Department of Energy Budget Activity Numbers KP 12 04 01 0 and KP.3334/CDIAC/atg.ndp001.2004 The Carbon Dioxide Research Group, Scripps Institution of Oceanography, UniversityNDP 001a ORNL/CDIAC-147 DOI: 10.3334/CDIAC/atg.ndp001.2004 Atmospheric Carbon Dioxide

  5. Atmospheric Trace Gases from the Carbon Dioxide Information Analysis Center (CDIAC)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    CDIAC products are indexed and searchable through a customized interface powered by ORNL's Mercury search engine. Products include numeric data packages, publications, trend data, atlases, models, etc. and can be searched for by subject area, keywords, authors, product numbers, time periods, collection sites, spatial references, etc. Some of the collections may also be included in the CDIAC publication, Trends Online: A Compendium of Global Change Data. Most data sets, many with numerous data files, are free to download from CDIAC's ftp area. The collections under the CDIAC heading of Atmospheric Trace Gases include: Atmospheric Carbon Dioxide, Atmospheric Methane, Atmospheric Carbon Monoxide, Atmospheric Hydrogen, Isotopes in Greenhouse Gases, Radionuclides, Aerosols, and Other Trace Gases.

  6. Variable temperature seat climate control system

    DOE Patents [OSTI]

    Karunasiri, Tissa R. (Van Nuys, CA); Gallup, David F. (Pasadena, CA); Noles, David R. (Glendale, CA); Gregory, Christian T. (Alhambra, CA)

    1997-05-06T23:59:59.000Z

    A temperature climate control system comprises a variable temperature seat, at least one heat pump, at least one heat pump temperature sensor, and a controller. Each heat pump comprises a number of Peltier thermoelectric modules for temperature conditioning the air in a main heat exchanger and a main exchanger fan for passing the conditioned air from the main exchanger to the variable temperature seat. The Peltier modules and each main fan may be manually adjusted via a control switch or a control signal. Additionally, the temperature climate control system may comprise a number of additional temperature sensors to monitor the temperature of the ambient air surrounding the occupant as well as the temperature of the conditioned air directed to the occupant. The controller is configured to automatically regulate the operation of the Peltier modules and/or each main fan according to a temperature climate control logic designed both to maximize occupant comfort during normal operation, and minimize possible equipment damage, occupant discomfort, or occupant injury in the event of a heat pump malfunction.

  7. Linear analysis of surface temperature dynamics and climate sensitivity

    E-Print Network [OSTI]

    Wu, Wei

    2007-04-25T23:59:59.000Z

    Spectral properties of global surface temperature and uncertainties of global climate sensitivity are explored in this work through the medium of Energy Balance Climate Models (EBCMs) and observational surface temperature data. In part I, a complete...

  8. Linear analysis of surface temperature dynamics and climate sensitivity 

    E-Print Network [OSTI]

    Wu, Wei

    2007-04-25T23:59:59.000Z

    Spectral properties of global surface temperature and uncertainties of global climate sensitivity are explored in this work through the medium of Energy Balance Climate Models (EBCMs) and observational surface temperature data. In part I, a complete...

  9. Global Carbon Budget from the Carbon Dioxide Information Analysis Center (CDIAC)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    The Global Carbon Project (GCP) was established in 2001 in recognition of the scientific challenge and critical importance of the carbon cycle for Earth's sustainability. The growing realization that anthropogenic climate change is a reality has focused the attention of the scientific community, policymakers and the general public on the rising concentration of greenhouse gases, especially carbon dioxide (CO2) in the atmosphere, and on the carbon cycle in general. Initial attempts, through the United Nations Framework Convention on Climate Change and its Kyoto Protocol, are underway to slow the rate of increase of greenhouse gases in the atmosphere. These societal actions require a scientific understanding of the carbon cycle, and are placing increasing demands on the international science community to establish a common, mutually agreed knowledge base to support policy debate and action. The Global Carbon Project is responding to this challenge through a shared partnership between the International Geosphere-Biosphere Programme (IGBP), the International Human Dimensions Programme on Global Environmental Change (IHDP), the World Climate Research Programme (WCRP) and Diversitas. This partnership constitutes the Earth Systems Science Partnership (ESSP). This CDIAC collection includes datasets, images, videos, presentations, and archived data from previous years.

  10. Trace Gas Emissions Data from the Carbon Dioxide Information Analysis Center (CDIAC)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    CDIAC products are indexed and searchable through a customized interface powered by ORNL's Mercury search engine. Products include numeric data packages, publications, trend data, atlases, and models and can be searched for by subject area, keywords, authors, product numbers, time periods, collection sites, spatial references, etc. Some of the collections may also be included in the CDIAC publication Trends Online: A Compendium of Global Change Data. Most data sets, many with numerous data files, are free to download from CDIAC's ftp area. Collections under the broad heading of Trace Gas Emissions are organized as Fossil-Fuel CO2 Emissions, Land-Use CO2 Emissions, Soil CO2 Emissions, and Methane.

  11. Land Use and Ecosystems Data from the Carbon Dioxide Information Analysis Center (CDIAC)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    CDIAC products are indexed and searchable through a customized interface powered by ORNL's Mercury search engine. Products include numeric data packages, publications, trend data, atlases, models, etc. and can be searched for by subject area, keywords, authors, product numbers, time periods, collection sites, spatial references, etc. Some of the collections may also be included in the CDIAC publication titled Trends Online: A Compendium of Global Change Data. Most data sets, many with numerous data files, are free to download from CDIAC's ftp area. Land Use and Ecosystems information includes Terrestrial Carbon Sequestration Data Sets, data sets from Africa and Asia, the Worldwide Organic Soil Carbon and Nitrogen Dataset, and much more.

  12. PACIFICA (PACIFic ocean Interior CArbon) Database: A Data Synthesis Resource (NDP-92, ORNL/CDIAC-159)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    Suzuki, T.; Ishii, M.; Aoyama, M. R; Christian, J. R.; Enyo, K.; Kawano, T.; Key, R. M.; Kosugi, N.; Kozyr, A.; Miller, L. A.; Murata, A.; Nakano, T.; Ono, T.; Saino, T.; Sasaki, K.; Sasano, D; Takatani, Y.; Wakita, M.; Sabine, C.

    PACIFICA (PACIFic ocean Interior CArbon) was an international collaborative project for synthesis of data on ocean interior carbon and its related parameters in the Pacific Ocean. The North Pacific Marine Science Organization (PICES), Section on Carbon and Climate (S-CC) supported the project. Hydrographic/hydrochemical datasets have been merged from a total of 272 cruises, including those from cruises conducted between the late 1980s and 2000 but not included in GLODAP, as well as CLIVAR/CO2 Repeat Hydrography datasets from the 2000s. Adjustments were calculated to account for analytical offsets in dissolved inorganic carbon, total alkalinity, salinity, oxygen, and nutrients (nitrate and nitrite, phosphate, and silicic acid) for each cruise as a result of the secondary quality control procedure, based on crossover analysis using data from deep layers (Tanhua et al., 2010). A total of 59 adjusted datasets from Line P off the west coast of Canada were also merged. Finally, the authors have produced the adjusted PACIFICA database that consists of datasets from a total of 306 cruises that also includes 34 datasets from WOCE Hydrographic Program cruises in the Pacific Ocean conducted in the 1990s. The PACIFICA database is available free of charge as a numeric data package (NDP-92) from the Carbon Dioxide Information Analysis Center (CDIAC) and the primary PACIFICA data site at pacifica.pices.jp. The NDP consists of the original cruise data files, adjusted data product, and the documentation.

  13. Terrestrial Carbon Management Data from the Carbon Dioxide Information Analysis Center (CDIAC)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    CDIAC products are indexed and searchable through a customized interface powered by ORNL's Mercury search engine. Products include numeric data packages, publications, trend data, atlases, and models and can be searched for by subject area, keywords, authors, product numbers, time periods, collection sites, spatial references, etc. Some of the collections may also be included in the CDIAC publication Trends Online: A Compendium of Global Change Data. Most data sets, many with numerous data files, are free to download from CDIAC's ftp area. Collections under the broad heading of Terrestrial Carbon Management are organized as Carbon Accumulation with Cropland Management, Carbon Accumulation with Grassland Management, Carbon Loss Following Cultivation, Carbon Accumulation Following Afforestation, and Carbon Sources and Sinks Associated with U.S. Cropland Production.

  14. CARINA (Carbon dioxide in the Atlantic Ocean) Data from CDIAC

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    The idea for CARINA developed at a workshop (CO2 in the northern North Atlantic) that was held at the HANSE-Wissenschaftskolleg (HANSE Institute for Advanced Study) in Delmenhorst, Germany from June 9 to 11, 1999. While the main scientific focus is the North Atlantic, some data from the South Atlantic have been included in the project, along with data from the Arctic Ocean. Data sets go back to 1972, and more than 100 are currently available. The data are also being used in conjunction with other projects and research groups, such as the Atlantic Ocean Carbon Synthesis Group. See the inventory of data at http://store.pangaea.de/Projects/CARBOOCEAN/carina/data_inventory.htm See a detailed table of information on the cruises at http://cdiac.ornl.gov/oceans/CARINA/Carina_table.html and also provides access to data files. The CARBOOCEAN data portal provides a specialized interface for CARINA data, a reference list for historic carbon data, and password protected access to the "Data Underway Warehouse.".

  15. ORNL/CDIAC-128 CARBON DIOXIDE, HYDROGRAPHIC, AND CHEMICAL DATA OBTAINED

    E-Print Network [OSTI]

    .S.A. Prepared by Alexander Kozyr1 Carbon Dioxide Information Analysis Center 1 Energy, Environment of Biological and Environmental Research U.S. Department of Energy Budget Activity Numbers KP 12 04 01 0 and KP#12;ORNL/CDIAC-128 NDP-075 CARBON DIOXIDE, HYDROGRAPHIC, AND CHEMICAL DATA OBTAINED DURING THE R

  16. ORNL/CDIAC-160 Climatological Distributions of pH, pCO2, Total CO2, Alkalinity,

    E-Print Network [OSTI]

    ORNL/CDIAC-160 NDP-094 Climatological Distributions of pH, pCO2, Total CO2, Alkalinity, and CaCO3, Alkalinity, and CaCO3 Saturation in the Global Surface Ocean. ORNL/CDIAC-160, NDP-094. Carbon Dioxide, total CO2 concentration (TCO2), and the degree of CaCO3 saturation for the global surface ocean waters

  17. Global Coastal Carbon Program Data from the Carbon Dioxide Information Analysis Center (CDIAC)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    CDIAC provides data management support for the Global Coastal Carbon Data Project. The coastal regions data are very important for the understanding of carbon cycle on the continental margins. The Coastal Project data include the bottle (discrete) and surface (underway) carbon-related measurements from coastal research cruises, the data from time series cruises, and coastal moorings. The data from US East Coast, US West Coast, and European Coastal areas are available. CDIAC provides a map interface with vessel or platform names. Clicking on the name brings up information about the vessel or the scientific platform, the kinds of measurements collected and the timeframe, links to project pages, when available, and the links to the data files themselves.

  18. Pace of shifts in climate regions increases with global temperature

    E-Print Network [OSTI]

    Mahlstein, Irina

    Human-induced climate change causes significant changes in local climates, which in turn lead to changes in regional climate zones. Large shifts in the world distribution of Köppen–Geiger climate classifications by the end ...

  19. Extracting CO2 from seawater: Climate change mitigation and renewable liquid fuel

    E-Print Network [OSTI]

    Homes, Christopher C.

    Extracting CO2 from seawater: Climate change mitigation and renewable liquid fuel Matthew Eisaman and their impact · Technology: Extracting CO2 from seawater · Application: Renewable liquid fuel #12;Outline: Renewable liquid fuel #12;The data on atmospheric CO2 2000 years ago http://cdiac.ornl.gov/trends/co2

  20. Variation in the sensitivity of organismal body temperature to climate change over local

    E-Print Network [OSTI]

    Gilman, Sarah

    climatic factors, including air temperature (Ta), surface temper- ature (Ts), solar radiation, cloud cover and communities (3­6). Accurately fore- casting the direct physiological effects of temperature change

  1. Impacts of Land-Use and Biofuels Policy on Climate: Temperature and Localized Impacts

    E-Print Network [OSTI]

    Impacts of Land-Use and Biofuels Policy on Climate: Temperature and Localized Impacts Willow on recycled paper #12;1 Impacts of Land-Use and Biofuels Policy on Climate: Temperature and Localized Impacts to agricultural production, including growing biofuels, and (ii) Observed Land Supply Response (OLSR

  2. The Global Historical Climatology Network: Long-term monthly temperature, precipitation, sea level pressure, and station pressure data

    SciTech Connect (OSTI)

    Vose, R.S. [Tennessee Univ., Knoxville, TN (United States). Energy, Environment and Resources Center; Schmoyer, R.L. [Oak Ridge National Lab., TN (United States); Steurer, P.M.; Peterson, T.C.; Heim, R.; Karl, T.R. [National Climatic Data Center, Asheville, NC (United States); Eischeid, J.K. [Colorado Univ., Boulder, CO (United States). Cooperative Inst. for Research in Environmental Sciences

    1992-07-01T23:59:59.000Z

    Interest in global climate change has risen dramatically during the last several years. In a similar fashion, the number of data sets available to study global change has also increased. Unfortunately, these data sets have been compiled by many different organizations/researchers, making it confusing and time consuming for individual researchers to acquire the ``best`` data. In response to this rapid growth in the number of global data sets, the Carbon Dioxide Information Analysis Center (CDIAC) and the National Climatic Data Center (NCDC) commenced the Global Historical Climatology Network (GHCN) project. The purpose of this project is to compile an improved global base-line data set of long-term monthly mean temperature, precipitation, sea level pressure, and station pressure for a dense network. of worldwide meteorological stations. Specifically, the GHCN project seeks to consolidate the numerous preexisting national-, regional-, and global-scale data sets into a single global climate data base that can be updated, enhanced, and distributed at regular intervals. The first version of the GHCN data base was completed during the summer of 1992. It contains 6039 temperature, 7533 precipitation, 1883 sea level pressure, and 1873 station pressure stations. All stations have at least 10 years of data, 40% have more than 50 years of data, and 10% have more than 100 years of data. Spatial coverage is good over most of the globe, particularly for the United States and central Europe. In comparison to other major global data sets, dramatic improvements are evident over South America, Africa, and Asia. The GHCN data base is available as a Numeric Data Package (NDP) from CDIAC. The NDP consists of this document and two magnetic tapes that contain machine-readable data files and accompanying retrieval codes. This document describes, in detail, both the GHCN data base and the contents of the magnetic tap

  3. The Global Historical Climatology Network: Long-term monthly temperature, precipitation, sea level pressure, and station pressure data

    SciTech Connect (OSTI)

    Vose, R.S. (Tennessee Univ., Knoxville, TN (United States). Energy, Environment and Resources Center); Schmoyer, R.L. (Oak Ridge National Lab., TN (United States)); Steurer, P.M.; Peterson, T.C.; Heim, R.; Karl, T.R. (National Climatic Data Center, Asheville, NC (United States)); Eischeid, J.K. (Colorado Univ., Boulder, CO (United States). Cooperative Inst. for Research in Environmental Sciences)

    1992-07-01T23:59:59.000Z

    Interest in global climate change has risen dramatically during the last several years. In a similar fashion, the number of data sets available to study global change has also increased. Unfortunately, these data sets have been compiled by many different organizations/researchers, making it confusing and time consuming for individual researchers to acquire the best'' data. In response to this rapid growth in the number of global data sets, the Carbon Dioxide Information Analysis Center (CDIAC) and the National Climatic Data Center (NCDC) commenced the Global Historical Climatology Network (GHCN) project. The purpose of this project is to compile an improved global base-line data set of long-term monthly mean temperature, precipitation, sea level pressure, and station pressure for a dense network. of worldwide meteorological stations. Specifically, the GHCN project seeks to consolidate the numerous preexisting national-, regional-, and global-scale data sets into a single global climate data base that can be updated, enhanced, and distributed at regular intervals. The first version of the GHCN data base was completed during the summer of 1992. It contains 6039 temperature, 7533 precipitation, 1883 sea level pressure, and 1873 station pressure stations. All stations have at least 10 years of data, 40% have more than 50 years of data, and 10% have more than 100 years of data. Spatial coverage is good over most of the globe, particularly for the United States and central Europe. In comparison to other major global data sets, dramatic improvements are evident over South America, Africa, and Asia. The GHCN data base is available as a Numeric Data Package (NDP) from CDIAC. The NDP consists of this document and two magnetic tapes that contain machine-readable data files and accompanying retrieval codes. This document describes, in detail, both the GHCN data base and the contents of the magnetic tap

  4. Detection and Attribution of Climate Change : From global mean temperature change to climate extremes and high impact weather.

    E-Print Network [OSTI]

    CERN. Geneva

    2013-01-01T23:59:59.000Z

    This talk will describe how evidence has grown in recent years for a human influence on climate and explain how the Fifth Assessment Report of the Intergovernmental Panel on Climate Change concluded that it is extremely likely (>95% probability) that human influence on climate has been the dominant cause of the observed global-mean warming since the mid-20th century. The fingerprint of human activities has also been detected in warming of the ocean, in changes in the global water cycle, in reductions in snow and ice, and in changes in some climate extremes. The strengthening of evidence for the effects of human influence on climate extremes is in line with long-held basic understanding of the consequences of mean warming for temperature extremes and for atmospheric moisture. Despite such compelling evidence this does not mean that every instance of high impact weather can be attributed to anthropogenic climate change, because climate variability is often a major factor in many locations, especially for rain...

  5. On the maintenance of weak meridional temperature gradients during warm climates

    E-Print Network [OSTI]

    Korty, Robert Lindsay

    2005-01-01T23:59:59.000Z

    This thesis examines the dynamics of equable climates. The underlying physics of two mechanisms by which weak meridional temperature gradients might be maintained are studied. First, I examine the evolution of stratospheric ...

  6. Research on the Temperature Control Method of an Artificial Climate Room 

    E-Print Network [OSTI]

    Jiang, Y.; Tan, W.; Wei, B.; Guo, R.

    2006-01-01T23:59:59.000Z

    An artificial climate room plays an important role in the research of an apparatus test and indoor/outdoor environment simulation. Generally, the refrigerator is used to decrease temperature to simulate outdoor environment, ...

  7. Sea surface temperature for climate from the along-track scanning radiometers 

    E-Print Network [OSTI]

    Embury, Owen

    2014-06-30T23:59:59.000Z

    This thesis describes the construction of a sea surface temperature (SST) dataset from Along-Track Scanning Radiometer (ATSR) observations suitable for climate applications. The algorithms presented here are now used at ...

  8. Research on the Temperature Control Method of an Artificial Climate Room

    E-Print Network [OSTI]

    Jiang, Y.; Tan, W.; Wei, B.; Guo, R.

    2006-01-01T23:59:59.000Z

    An artificial climate room plays an important role in the research of an apparatus test and indoor/outdoor environment simulation. Generally, the refrigerator is used to decrease temperature to simulate outdoor environment, while a heater is used...

  9. Oceanic Trace Gases Numeric Data Packages from the Carbon Dioxide Information Analysis Center (CDIAC)

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    CDIAC products include numeric data packages, publications, trend data, atlases, models, etc. and can be searched for by subject area, keywords, authors, product numbers, time periods, collection sites, spatial references, etc. Most data sets or packages, many with numerous data files, are free to download from CDIAC's ftp area. CDIAC lists the following numeric data packages under the broad heading of Oceanic Trace Gases: Carbon Dioxide, Hydrographic, and Chemical Data Obtained during the R/V Ronald H. Brown Repeat Hydrography Cruise in the Atlantic Ocean: CLIVAR CO2 Section A16S_2005 ( 01/11/05 - 022405) • Determination of Carbon Dioxide, Hydrographic, and Chemical Parameters during the R/V Nathaniel B. Palmer Cruise in the Southern Indian Ocean (WOCE Section S04I, 050396 - 070496) • Inorganic Carbon, Nutrient, and Oxygen Data from the R/V Ronald H. Brown Repeat Hydrography Cruise in the Atlantic Ocean: CLIVAR CO2 Section A16N_2003a (060403 – 081103) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Maurice Ewing Cruise in the Atlantic Ocean (WOCE Section A17, 010494 - 032194) • Global Ocean Data Analysis Project GLODAP: Results and Data • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Knorr Cruises in the North Atlantic Ocean on WOCE Sections AR24 (1102 – 120596) and A24, A20, and A22 (053097 – 090397) • Carbon Dioxide, Hydrographic and Chemical Data Obtained During the Nine R/V Knorr Cruises Comprising the Indian Ocean CO2 Survey (WOCE Sections I8SI9S, I9N, I8NI5E, I3, I5WI4, I7N, I1, I10, and I2; 120 194 – 012296) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Meteor Cruise 28/1 in the South Atlantic Ocean (WOCE Section A8, 032994 - 051294) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Knorr Cruise 138-3, -4, and -5 in the South Pacific Ocean (WOCE Sections P6E, P6C, and P6W, 050292 - 073092) • Global Distribution of Total Inorganic Carbon and Total Alkalinity below the deepest winter mixed layer depths • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V John V. Vickers Cruise in the Pacific Ocean (WOCE Section P13, NOAA CGC92 Cruise, 080492 – 102192) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Hesperides Cruise in the Atlantic Ocean (WOCE Section A5, 071492 - 081592) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Thomas G. Thompson Cruise in the Pacific Ocean (WOCE Section P10, 100593 – 111093) • The International Intercomparison Exercise of Underway fCO2 Systems during the R/V Meteor Cruise 36/1 in the North Atlantic Ocean • Carbon Dioxide, Hydrographic, and Chemical Data Obtained during the R/V Meteor Cruise 22/5 in the South Atlantic Ocean (WOCE Section A10, Dec. 1992-Jan, 1993) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained in the South Pacific Ocean (WOCE Sections P16A/P17A, P17E/P19S, and P19C, R/V Knorr , Oct. 1992-April 1993) • Surface Water and Atmospheric Underway Carbon Data Obtained During the World Ocean Circulation Experiment Indian Ocean Survey Cruises (R/V Knorr, Dec. 1994 – Jan, 1996) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Akademik Ioffe Cruise in the South Pacific Ocean (WOCE Section S4P, Feb.-April 1992) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Thomas Washington Cruise TUNES-1 in the Equatorial Pacific Ocean (WOCE section P17C) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Thomas Washington Cruise TUNES-3 in the Equatorial Pacific Ocean (WOCE section P16C) • Carbon-14 Measurements in Surface Water CO2 from the Atlantic, Indian and Pacific Oceans, 1965-1994 • Carbon Dioxide, Hydrographic, and Chemical Data Obtained During R/V Meteor Cruise 18/1 in the North Atlantic Ocean (WOCE Section A1E) • Carbon Dioxide, Hydrographic, and Chemical Data Obtained in the Central South Pacific Ocean (WOCE Sections P17S and P16S) during the TUNES-2 Expedition of the R/V Th

  10. CDIAC -WHPO/CCHDO Data Management Plan for CTD/Hydrographic/CO2/Tracer Data for the Global Ocean Carbon and

    E-Print Network [OSTI]

    Carbon and Repeat Hydrography Program Alex Kozyr Carbon Dioxide Information Analysis Center Environmental://cdiac.esd.ornl.gov/oceans/home.html James H. Swift WOCE Hydrographic Program Office (CLIVAR and Carbon Hydrographic Data Office) UCSD oceanographic research depends on the availability and clarity of existing data. Two data offices in the US deal

  11. ORNL/CDIAC-145 GLOBAL OCEAN DATA ANALYSIS PROJECT (GLODAP): RESULTS AND DATA

    E-Print Network [OSTI]

    and Environmental Research U.S. Department of Energy Budget Activity Numbers KP 12 04 01 0 and KP 12 02 03 0.S.A. 3 Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, DOE, Oak Ridge, TN, U Published: August 2005 Prepared for the Climate Change Research Division Office of Biological

  12. Low Frequency Modulation of Extreme Temperature Regimes in a Changing Climate

    SciTech Connect (OSTI)

    Black, Robert X.

    2014-11-24T23:59:59.000Z

    The project examines long-term changes in extreme temperature episodes (ETE) associated with planetary climate modes (PCMs) in both the real atmospheric and climate model simulations. The focus is on cold air outbreaks (CAOs) and warm waves (WWs) occurring over the continental US during the past 60 winters. No significant long-term trends in either WWs or CAOs are observed over the US. The annual frequency of CAOs is affected by the (i) North Atlantic Oscillation (NAO) over the Southeast US and (ii) Pacific–North American (PNA) pattern over the Northwest US. WW frequency is influenced by the (i) NAO over the eastern US and (ii) combined influence of PNA, Pacific decadal oscillation (PDO), and ENSO over the southern US. The collective influence of PCMs accounts for as much as 50% of the regional variability in ETE frequency. During CAO (WW) events occurring over the southeast US, there are low (high) pressure anomalies at higher atmospheric levels over the southeast US with oppositely-signed pressure anomalies in the lower atmosphere over the central US. These patterns lead to anomalous northerly (for CAOs) or southerly (for WWs) flow into the southeast leading to cold or warm surface air temperature anomalies, respectively. One distinction is that CAOs involve substantial air mass transport while WW formation is more local in nature. The primary differences among event categories are in the origin and nature of the pressure anomaly features linked to ETE onset. In some cases, PCMs help to provide a favorable environment for event onset. Heat budget analyses indicate that latitudinal transport in the lower atmosphere is the main contributor to regional cooling during CAO onset. This is partly offset by adiabatic warming associated with subsiding air. Additional diagnoses reveal that this latitudinal transport is partly due to the remote physical influence of a shallow cold pool of air trapped along the east side of the Rocky Mountains. ETE and PCM behavior is also studied in (CMIP5) climate model simulations. Although the climate models considered are able to represent the overall behavior of ETEs, the frequency of WWs (CAOs) is too high (low) in many models. While all models qualitatively replicate the overall structure of the PNA pattern, a small minority of models fails to properly simulate the NAO pattern. Model shortcomings in representing the NAO and PNA patterns have important consequences for simulating associated regional variability in surface air temperature and storm track behavior. The influence of PCMs on ETEs is underestimated in most CMIP5 models. In particular, none of the models are able to accurately simulate observed linkages between ETEs and the PDO, due to a gross misrepresentation of the PDO pattern in most models. Our results indicate that predictions of future CAO and WW behavior are currently limited by the ability of climate models to accurately represent PCM characteristics. Our study also considers the behavior of PCMs known as annular modes. It is determined that north-south movements in the stratospheric jet stream (related to the Polar Annular Mode) result in long-lasting impacts upon surface weather conditions including regional air temperature anomalies. The structure and dynamics of the stratospheric northern annular mode (or SNAM, related to changes in the strength of the stratospheric jet stream) was studied in CMIP5 models. In models with poorly-resolved stratospheres, the amplitude of SNAM at stratospheric altitudes is typically too weak, consistent with weaker stratospheric jet variability. However, this distinction does not carry over to the associated tropospheric signature of SNAM. A regional analysis illustrates that most CMIP5 models (regardless of whether the stratosphere is well-resolved) have anomalously weak and eastward shifted (compared to observed SNAM events) storm track and sea level pressure anomaly patterns during SNAM events. Analyses of stratosphere–troposphere coupling reveal that large-scale wave activity in the stratosphere is anomalously weak in CMIP5 model

  13. Testing for the Possible Influence of Unknown Climate Forcings upon Global Temperature Increases from 1950-2000

    SciTech Connect (OSTI)

    Anderson, Bruce T.; Knight, Jeff R.; Ringer, Mark A.; Yoon, Jin-Ho; Cherchi, Annalisa

    2012-10-15T23:59:59.000Z

    Global-scale variations in the climate system over the last half of the twentieth century, including long-term increases in global-mean near-surface temperatures, are consistent with concurrent human-induced emissions of radiatively active gases and aerosols. However, such consistency does not preclude the possible influence of other forcing agents, including internal modes of climate variability or unaccounted for aerosol effects. To test whether other unknown forcing agents may have contributed to multidecadal increases in global-mean near-surface temperatures from 1950 to 2000, data pertaining to observed changes in global-scale sea surface temperatures and observed changes in radiatively active atmospheric constituents are incorporated into numerical global climate models. Results indicate that the radiative forcing needed to produce the observed long-term trends in sea surface temperatures—and global-mean near-surface temperatures—is provided predominantly by known changes in greenhouse gases and aerosols. Further, results indicate that less than 10% of the long-term historical increase in global-mean near-surface temperatures over the last half of the twentieth century could have been the result of internal climate variability. In addition, they indicate that less than 25%of the total radiative forcing needed to produce the observed long-term trend in global-mean near-surface temperatures could have been provided by changes in net radiative forcing from unknown sources (either positive or negative). These results, which are derived from simple energy balance requirements, emphasize the important role humans have played in modifying the global climate over the last half of the twentieth century.

  14. HIPPO (HIAPER Pole-to-Pole Observations) Data from CDIAC's HIPPO Data Archive

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    The HIPPO (HIAPER Pole-to-Pole Observations) study of the carbon cycle and greenhouse gases measured meteorology, atmospheric chemistry, and aerosol constituents along transects from approximately pole-to-pole over the Pacific Ocean. HIPPO flew hundreds of vertical profiles from the ocean/ice surface to as high as the tropopause, at five times during different seasons over a three year period from 2009-2011. HIPPO provides the first high-resolution vertically-resolved global survey of a comprehensive suite of atmospheric trace gases and aerosols pertinent to understanding the carbon cycle and challenging global climate models.

  15. Temperature effects induced by climate change on the growth and consumption by salmonines in Lakes Michigan and Huron

    E-Print Network [OSTI]

    2014 Abstract We used bioenergetics models to investigate temperature effects induced by climate change (1964­1993) and projected in the future period (2043­2070). Bioenergetics simula- tions were run across change . Bioenergetics models . Salmonines . Lake michigan . Lake huron Introduction Following the global

  16. Lifetime of Anthropogenic Climate Change: Millennial Time Scales of Potential CO2 and Surface Temperature Perturbations

    E-Print Network [OSTI]

    Scherer, Norbert F.

    ). Earth system models can be used to simulate the ev- olution of the climate system under different anthro

  17. Elevated air temperature alters an old-field insect community in a multi-factor climate change experiment

    SciTech Connect (OSTI)

    Villalpando, Sean [Appalachian State University; Williams, Ray [ORNL; Norby, Richard J [ORNL

    2009-01-01T23:59:59.000Z

    To address how multiple, interacting climate drivers may affect plant-insect community associations, we sampled the insect community from a constructed old-field plant community grown under simultaneous [CO2], temperature, and water manipulation. Insects were identified to morphospecies, assigned to feeding guilds and abundance, richness and evenness quantified. Warming significantly increased Order Thysanoptera abundance and reduced overall morphospecies richness and evenness. Non-metric multidimensional scaling clearly supported the effect of warming on insect community composition. Reductions in richness for herbivores and parasitoids suggest trophic-level effects within the insect community. Analysis of dominant insects demonstrated the effects of warming were limited to a relatively small number of morphospecies. Reported reductions in whole-community foliar N at elevated [CO2] unexpectedly did not result in any effects on herbivores. These results demonstrate climatic warming may alter certain insect communities via effects on insect species most responsive to higher temperature, contributing to a change in community structure.

  18. The bi-variate frequency distribution of two concurrent climatic variables: a study of temperature and dew point 

    E-Print Network [OSTI]

    Zeitler, Jon William

    1991-01-01T23:59:59.000Z

    Study of Temperature and Dew Point (December 1991). Jon William Zeitler, B. S. , iowa State University Chair of Advisory Comminee; Prof. John F. Griffiths The bi-variate normal distribution was fitted for the mid-season months of January, April, July... as to style and content by: Jo F. Griffnhs "' (Chair of Committee) Robert C. Runnels (Member) J. ' e (Mem r) Edward J. ser (Head of Department) December 1991 ABSTRACT The Bi-Variate Frequency Distribution of Two Concurrent Climatic Variables: A...

  19. Q&A on "Impacts of Wind Farms on Land Surface Temperature" Published by Nature Climate Change on April 29, 2012

    E-Print Network [OSTI]

    Zhou, Liming

    1 Q&A on "Impacts of Wind Farms on Land Surface Temperature" Published by Nature Climate Change? This study presents the first observational evidence of wind farm impacts on land surface temperature downwind of wind farms. Why do the operating wind turbines warm nighttime temperature? This warming effect

  20. Climate Systems and Climate Change Is Climate Change Real?

    E-Print Network [OSTI]

    Pan, Feifei

    Chapter 10 Climate Systems and Climate Change #12;Is Climate Change Real? 1980 1898 2005 2003 #12;Arctic Sea Ice Changes #12;Observed Global Surface Air Temperature #12;! Current climate: weather station data, remote sensing data, numerical modeling using General Circulation Models (GCM) ! Past climate

  1. Impacts of Land Use and Biofuels Policy on Climate: Temperature and Localized Impacts

    E-Print Network [OSTI]

    Hallgren, Willow

    2012-08-06T23:59:59.000Z

    The impact on climate of future land use and energy policy scenarios is explored using two landuse frameworks: (i) Pure Cost Conversion Response (PCCR), or 'extensification', where the price of land is the only constraint ...

  2. 3D modelling of the early Martian Climate under a denser CO2 atmosphere: Temperatures and CO2 ice clouds

    E-Print Network [OSTI]

    Forget, Francois; Millour, Ehouarn; Madeleine, Jean-Baptiste; Kerber, Laura; Leconte, Jeremy; Marcq, Emmanuel; Haberle, Robert M

    2012-01-01T23:59:59.000Z

    On the basis of geological evidence, it is often stated that the early martian climate was warm enough for liquid water to flow on the surface thanks to the greenhouse effect of a thick atmosphere. We present 3D global climate simulations of the early martian climate performed assuming a faint young sun and a CO2 atmosphere with pressure between 0.1 and 7 bars. The model includes a detailed radiative transfer model using revised CO2 gas collision induced absorption properties, and a parameterisation of the CO2 ice cloud microphysical and radiative properties. A wide range of possible climates is explored by using various values of obliquities, orbital parameters, cloud microphysic parameters, atmospheric dust loading, and surface properties. Unlike on present day Mars, for pressures higher than a fraction of a bar, surface temperatures vary with altitude because of the adiabatic cooling and warming of the atmosphere when it moves vertically. In most simulations, CO2 ice clouds cover a major part of the planet...

  3. Greenland temperature, climate change, and human society during the last 11,600 years

    E-Print Network [OSTI]

    Kobashi, Takuro

    2007-01-01T23:59:59.000Z

    temperature reconstruction from water isotopes in ice cores.temperature reconstruction from water isotopes in ice cores,Finkel, Changes in deep-water formation during the Younger

  4. Greenland temperature, climate change, and human society during the last 11,600 years

    E-Print Network [OSTI]

    Kobashi, Takuro

    2007-01-01T23:59:59.000Z

    temperatures directly from the Greenland Ice Sheet. Science2006. The 8.2ka event from Greenland ice cores. QuaternaryJouzel, Isotope calibrated Greenland temperature record over

  5. Effect of ocean temperature on southwestern U.S. climate analyzed

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Environmental Visualization Laboratory depicts sea surface temperatures around Greenland from October 2010. Image from National Oceanic and Atmospheric Administration's...

  6. Effect of ocean temperature on southwestern U.S. climate analyzed

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    LANL's Space and Remote Sensing group led the scientists to perform multiple linear regression analysis of surface air temperature and precipitation records provided by the...

  7. Effects of white roofs on urban temperature in a global climate model

    E-Print Network [OSTI]

    Oleson, Keith W.; Bonan, Gordon B.; Feddema, Johannes J.

    2010-02-01T23:59:59.000Z

    over all urban areas, the annual mean heat island decreased by 33%. Urban daily maximum temperature decreased by 0.6°C and daily minimum temperature by 0.3°C. Spatial variability in the heat island response is caused by changes in absorbed solar...

  8. Effects of upstream dams versus groundwater pumping on stream temperature under varying climate conditions

    E-Print Network [OSTI]

    Click Here for Full Article Effects of upstream dams versus groundwater pumping on stream impact of a large upstream dam versus inreach groundwater pumping on stream temperatures was analyzed large dams are present, such as the western United States or eastern Australia. Stream temperatures were

  9. Distribution of Soil Temperature Regimes and Climate Change in the Mojave Desert Region

    E-Print Network [OSTI]

    Bai, Yanying

    2009-01-01T23:59:59.000Z

    precipitation, and water vapor on diurnal temperature range.Idaho, United States. Water Resour. Res. 37: 2843-2846.and J. Bouma. 1994. Modelling water and chemical fluxes as

  10. Experimental short-term climate forecasting procedure for US winter temperatures and its verification

    SciTech Connect (OSTI)

    Navato, A.R.

    1981-01-01T23:59:59.000Z

    A linear multivariate regression model for continental United States Januray surface air temperatures is presented. The predictors enter the regression equation at more than one lag if their effects on the predictand tend to be spread over several months rather than be completed in one month. The monthly mean surface tempertures for 12 cities were taken to be representative of temperatures for the regions around them. The predictand series then consisted of annual January values for each representative city. A separate regression equation was derived for the annual departures from the long term means for January for each city. The procedure therefore predicts the inter-annual variability for January. The regression equations for inter-annual variability were able to explain a much higher percentage of variance compared to the corresponding regression equations for monthly variability. The same procedure can be applied to obtain prediction equations for other months. The higher percentage is to be expected if it is considered that there must be differences in the operation of temperature-controlling physical mechanisms which are dependent on the march of the seasons.

  11. Collaborative Research: Process-Resolving Decomposition of the Global Temperature Response to Modes of Low Frequency Variability in a Changing Climate

    SciTech Connect (OSTI)

    Deng, Yi

    2014-11-24T23:59:59.000Z

    DOE-GTRC-05596 11/24/2104 Collaborative Research: Process-Resolving Decomposition of the Global Temperature Response to Modes of Low Frequency Variability in a Changing Climate PI: Dr. Yi Deng (PI) School of Earth and Atmospheric Sciences Georgia Institute of Technology 404-385-1821, yi.deng@eas.gatech.edu El Niño-Southern Oscillation (ENSO) and Annular Modes (AMs) represent respectively the most important modes of low frequency variability in the tropical and extratropical circulations. The projection of future changes in the ENSO and AM variability, however, remains highly uncertain with the state-of-the-science climate models. This project conducted a process-resolving, quantitative evaluations of the ENSO and AM variability in the modern reanalysis observations and in climate model simulations. The goal is to identify and understand the sources of uncertainty and biases in models’ representation of ENSO and AM variability. Using a feedback analysis method originally formulated by one of the collaborative PIs, we partitioned the 3D atmospheric temperature anomalies and surface temperature anomalies associated with ENSO and AM variability into components linked to 1) radiation-related thermodynamic processes such as cloud and water vapor feedbacks, 2) local dynamical processes including convection and turbulent/diffusive energy transfer and 3) non-local dynamical processes such as the horizontal energy transport in the oceans and atmosphere. In the past 4 years, the research conducted at Georgia Tech under the support of this project has led to 15 peer-reviewed publications and 9 conference/workshop presentations. Two graduate students and one postdoctoral fellow also received research training through participating the project activities. This final technical report summarizes key scientific discoveries we made and provides also a list of all publications and conference presentations resulted from research activities at Georgia Tech. The main findings include: 1) the distinctly different roles played by atmospheric dynamical processes in establishing surface temperature response to ENSO at tropics and extratropics (i.e., atmospheric dynamics disperses energy out of tropics during ENSO warm events and modulate surface temperature at mid-, high-latitudes through controlling downward longwave radiation); 2) the representations of ENSO-related temperature response in climate models fail to converge at the process-level particularly over extratropics (i.e., models produce the right temperature responses to ENSO but with wrong reasons); 3) water vapor feedback contributes substantially to the temperature anomalies found over U.S. during different phases of the Northern Annular Mode (NAM), which adds new insight to the traditional picture that cold/warm advective processes are the main drivers of local temperature responses to the NAM; 4) the overall land surface temperature biases in the latest NCAR model (CESM1) are caused by biases in surface albedo while the surface temperature biases over ocean are related to multiple factors including biases in model albedo, cloud and oceanic dynamics, and the temperature biases over different ocean basins are also induced by different process biases. These results provide a detailed guidance for process-level model turning and improvement, and thus contribute directly to the overall goal of reducing model uncertainty in projecting future changes in the Earth’s climate system, especially in the ENSO and AM variability.

  12. Influence of climate model biases and daily-scale temperature and precipitation events on hydrological impacts assessment: A case study of the United States

    SciTech Connect (OSTI)

    Ashfaq, Moetasim [ORNL; Bowling, Laura C. [Purdue University; Cherkauer, Keith [Purdue University; Pal, Jeremy [Loyola University; Diffenbaugh, Noah [Stanford University

    2010-01-01T23:59:59.000Z

    The Intergovernmental Panel on Climate Change's Fourth Assessment Report concludes that climate change is now unequivocal, and associated increases in evaporation and atmospheric water content could intensify the hydrological cycle. However, the biases and coarse spatial resolution of global climate models limit their usefulness in hydrological impact assessment. In order to reduce these limitations, we use a high-resolution regional climate model (RegCM3) to drive a hydrological model (variable infiltration capacity) for the full contiguous United States. The simulations cover 1961-1990 in the historic period and 2071-2100 in the future (A2) period. A quantile-based bias correction technique is applied to the times series of RegCM3-simulated precipitation and temperature. Our results show that biases in the RegCM3 fields not only affect the magnitude of hydrometeorological variables in the baseline hydrological simulation, but they also affect the response of hydrological variables to projected future anthropogenic increases in greenhouse forcing. Further, we find that changes in the intensity and occurrence of severe wet and hot events are critical in determining the sign of hydrologic change. These results have important implications for the assessment of potential future hydrologic changes, as well as for developing approaches for quantitative impacts assessment.

  13. AMPLIFIED GREENHOUSE EFFECT SHAPING NORTH INTO SOUTH A new study published in Nature Climate Change reports decreasing temperature

    E-Print Network [OSTI]

    Myneni, Ranga B.

    AMPLIFIED GREENHOUSE EFFECT SHAPING NORTH INTO SOUTH A new study published in Nature Climate Change. A greenhouse effect initiated by increased atmospheric concentration of heat-trapping gasses, such as water greenhouse effect. This amplified warming in the North, roughly above the border between Canada and the USA

  14. Spatial and temporal climate variations influencing medium-range temperature predictions over south-central European Russia

    E-Print Network [OSTI]

    Johnson, Jeffrey Edward

    1990-01-01T23:59:59.000Z

    JOHNSON Approved as to style and content by: ohn F. Gri hs tChair of Cotnmittee) Steven W. L ons t 1VIember) . J. Freund Member) James R. Scoggins tHead of Department) May 1990 ABSTRACT Spatial and Temporal Climate Variations Influencing Medium... det. ailed climatology. A monthly overview f' or 9 stations in the region is given for the weather elements as stated above. Pentad and 3-hourly averages are also included. The detailed climatology is helpful in orienting a. new weather forecaster...

  15. Comment on "Methodology and results of calculating Central California surface temperature trends: evidence of human-induced climate change?" by Christy et al. (2006)

    SciTech Connect (OSTI)

    Bonfils, C; Duffy, P; Lobell, D

    2006-03-28T23:59:59.000Z

    Understanding the causes of observed regional temperature trends is essential to projecting the human influences on climate, and the societal impacts of these influences. In their recent study, Christy et al. (2006, hereinafter CRNG06) hypothesized that the presence of irrigated soils is responsible for rapid warming of summer nights occurring in California's Central Valley over the last century (1910-2003), an assumption that rules out any significant effect due to increased greenhouse gases, urbanization, or other factors in this region. We question this interpretation, which is based on an apparent contrast in summer nighttime temperature trends between the San Joaquin Valley ({approx} +0.3 {+-} 0.1 C/decade) and the adjacent western slopes of the Sierra Nevada (-0.25 {+-} 0.15 C/decade), as well as the amplitude, sign and uncertainty of the Sierra nighttime temperature trend itself. We, however, do not dispute the finding of other Sierra and Valley trends. Regarding the veracity of the apparent Sierra nighttime temperature trend, CRNG06 generated the Valley and Sierra time-series using a meticulous procedure that eliminates discontinuities and isolates homogeneous segments in temperature records from 41 weather stations. This procedure yields an apparent cooling of about -0.25 {+-} 0.15 C/decade in the Sierra region. However, because removal of one of the 137 Sierra segments, from the most elevated site (Huntington Lake, 2140m), causes an increase in nighttime temperature trend as large as the trend itself (of +0.25 C/decade, CH06), and leads to a zero trend, the apparent cooling of summer nights in the Sierra regions seems, in fact, largely uncertain.

  16. Applications of statistical models to synchronous climate variables: a case study of temperature and dew point for College Station, Texas 

    E-Print Network [OSTI]

    O'Brien, Charles F.

    1995-01-01T23:59:59.000Z

    transformations. Generally speaking, temperature, dew point, and dew point depression values could be transformed to resemble a bivariate normal distribution. Of the 288 cases (6 mos. x 24 hrs. x 2 moisture variables) applied to the bivariate normal distribution...

  17. Modeled Interactive Effects of Precipitation, temperature, and [CO2] on Ecosystem Carbon and Water Dynamics in Different Climatic Zones

    SciTech Connect (OSTI)

    Luo, Yiqi [University of Oklahoma; Gerten, Dieter [Potsdam Institute for Climate Impact Research, Potsdam, Germany; Le Maire, Guerric [Laboratoire des Sciences du Climat et de l'Environement, France; Parton, William [University of Colorado, Fort Collins; Weng, Ensheng [University of Oklahoma, Norman; Zhou, Xuhuui [University of Oklahoma; Keough, Cindy [University of Colorado, Fort Collins; Beier, Claus [Riso National Laboratory, Roskilde, Denmark; Ciais, Philippe [Laboratoire des Sciences du Climat et de l'Environement, France; Cramer, Wolfgang [Potsdam Institute for Climate Impact Research, Potsdam, Germany; Dukes, Jeff [University of Massachusetts, Boston; Emmett, Bridget [Centre for Ecology and Hydrology, Bangor, Gwynedd, United Kingdom; Hanson, Paul J [ORNL; Knapp, Alan [Colorado State University, Fort Collins; Linder, Sune [Swedish University of Agricultural Sciences, Upsalla, Sweden; Nepstad, Daniel [Woods Hole Oceanographic Institution (WHOI), Woods Hole, MA; Rustad, Lindsey [USDA Forest Service

    2008-01-01T23:59:59.000Z

    Interactive effects of multiple global change factors on ecosystem processes are complex. It is relatively expensive to explore those interactions in manipulative experiments. We conducted a modeling analysis to identify potentially important interactions and to stimulate hypothesis formulation for experimental research. Four models were used to quantify interactive effects of climate warming (T), altered precipitation amounts [doubled (DP) and halved (HP)] and seasonality (SP, moving precipitation in July and August to January and February to create summer drought), and elevated [CO2] (C) on net primary production (NPP), heterotrophic respiration (Rh), net ecosystem production (NEP), transpiration, and runoff.We examined those responses in seven ecosystems, including forests, grasslands, and heathlands in different climate zones. The modeling analysis showed that none of the threeway interactions among T, C, and altered precipitation was substantial for either carbon or water processes, nor consistent among the seven ecosystems. However, two-way interactive effects on NPP, Rh, and NEP were generally positive (i.e. amplification of one factor s effect by the other factor) between T and C or between T and DP. A negative interaction (i.e. depression of one factor s effect by the other factor) occurred for simulated NPP between T and HP. The interactive effects on runoff were positive between T and HP. Four pairs of two-way interactive effects on plant transpiration were positive and two pairs negative. In addition, wet sites generally had smaller relative changes in NPP, Rh, runoff, and transpiration but larger absolute changes in NEP than dry sites in response to the treatments. The modeling results suggest new hypotheses to be tested in multifactor global change experiments. Likewise, more experimental evidence is needed for the further improvement of ecosystem models in order to adequately simulate complex interactive processes.

  18. Climate and weather events can impact human health in many ways. Climate trends, such as warming temperatures and changes in precipitation patterns, can affect the distribution of waterborne and vector-borne

    E-Print Network [OSTI]

    and mortality. Providing access to relevant climate information is essential to understanding how climate trends. · Using relative humidity and wind speed data to study the relationship between fine particulate air pollution and daily mortality counts. NOAA's National Climatic Data Center Sectoral Engagement Fact Sheet

  19. We already have clear evidence for climate change with a 0.75C rise in global temperatures

    E-Print Network [OSTI]

    Jones, Peter JS

    and use energy in the UK and theWorld. The greenhouse The temperature of the Earth is determined by the balance between energy from the sun and its loss back into space. Most of the incoming solar short `light') passes through the atmosphere without interference. About one-third of the solar energy

  20. Soil moisture surpasses elevated CO2 and temperature as a control on soil carbon dynamics in a multi-factor climate change experiment

    SciTech Connect (OSTI)

    Garten Jr, Charles T [ORNL; Classen, Aimee T [ORNL; Norby, Richard J [ORNL

    2009-01-01T23:59:59.000Z

    Some single-factor experiments suggest that elevated CO2 concentrations can increase soil carbon, but few experiments have examined the effects of interacting environmental factors on soil carbon dynamics. We undertook studies of soil carbon and nitrogen in a multi-factor (CO2 x temperature x soil moisture) climate change experiment on a constructed old-field ecosystem. After four growing seasons, elevated CO2 had no measurable effect on carbon and nitrogen concentrations in whole soil, particulate organic matter (POM), and mineral-associated organic matter (MOM). Analysis of stable carbon isotopes, under elevated CO2, indicated between 14 and 19% new soil carbon under two different watering treatments with as much as 48% new carbon in POM. Despite significant belowground inputs of new organic matter, soil carbon concentrations and stocks in POM declined over four years under soil moisture conditions that corresponded to prevailing precipitation inputs (1,300 mm yr-1). Changes over time in soil carbon and nitrogen under a drought treatment (approximately 20% lower soil water content) were not statistically significant. Reduced soil moisture lowered soil CO2 efflux and slowed soil carbon cycling in the POM pool. In this experiment, soil moisture (produced by different watering treatments) was more important than elevated CO2 and temperature as a control on soil carbon dynamics.

  1. Climate Action Plan (Vermont)

    Broader source: Energy.gov [DOE]

    There is a growing scientific consensus that increasing emissions of greenhouse gases to the atmosphere are affecting the temperature and variability of the Earth’s climate. Recognizing the...

  2. avoid climate change: Topics by E-print Network

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Climate Change Real? 1980 1898 2005 2003 12;Arctic Sea Ice Changes 12;Observed Global Surface Air Temperature 12; Current climate: weather station data, remote sensing...

  3. The Climate of the South Platte Basin

    E-Print Network [OSTI]

    The Climate of the South Platte Basin Colorado Climate Center http://climate.atmos.colostate.edu #12;Key Features of the Climate of the South Platte Basin #12;Temperature Cold winters Hot summers #12;Precipitation Monthly Average Precipitation for Selected Sites in the South Platte Basin 0.00 0

  4. ProGreen 2014 Colorado Climate Update

    E-Print Network [OSTI]

    · Complex Mountain topography · Solar energy and seasonal cycles drive our climate #12;Colorado has" and we LOVE IT! #12;Monitoring our Climate · Elements: temperature, precipitation, snow, wind, solarProGreen 2014 Colorado Climate Update Nolan Doesken Colorado State Climatologist Colorado Climate

  5. Climate Science and Drought

    E-Print Network [OSTI]

    Gordon, W.

    2011-01-01T23:59:59.000Z

    Texas Climate Change and Drought Wendy Gordon, Ph.D. The University of Texas ? Austin Environmental Science Institute Texas Wildfires 2011 From the beginning of the fire season on November 15, 2010 to October 31, 2011 nearly 28,000 fires had... have been particularly severe due to the ongoing 2011 Southern US drought, and exacerbating the problem is land management practices, the unusual convergence of strong winds, unseasonably warm temperatures, and low humidity. Climate...

  6. Questions of bias in climate models

    SciTech Connect (OSTI)

    Smith, Steven J.; Wigley, Tom M.; Meinshausen, Malte; Rogelj, Joeri

    2014-08-27T23:59:59.000Z

    The recent work by Shindell usefully contributes to the debate over estimating climate sensitivity by highlighting an important aspect of the climate system: that climate forcings that occur over land result in a more rapid temperature response than forcings that are distributed more uniformly over the globe. While, as noted in this work, simple climate models may be biased by assuming the same temperature response for all forcing agents, the implication that the MAGICC model is biased in this way is not correct.

  7. Carbon Dioxide Information Analysis Center and World Data Center-A for atmospheric trace gases: FY 1993 activities

    SciTech Connect (OSTI)

    Cushman, R.M. [Oak Ridge National Lab., TN (United States). Carbon Dioxide Information Analysis Center; Stoss, F.W. [Oak Ridge National Lab., TN (United States). Carbon Dioxide Information Analysis Center]|[Univ. of Tennessee, Knoxville, TN (United States). Energy, Environment, and Resources Center

    1994-01-01T23:59:59.000Z

    During the course of a fiscal year, Oak Ridge National Laboratory`s Carbon Dioxide Information Analysis Center (CDIAC) distributes thousands of specialty publications-numeric data packages (NDPs), computer model packages (CMPs), technical reports, public communication publications, newsletters, article reprints, and reference books-in response to requests for information related to global environmental issues, primarily those pertaining to climate change. CDIAC`s staff also provide technical responses to specific inquiries related to carbon dioxide (CO{sub 2}), other trace gases, and climate. Hundreds of referrals to other researchers, policy analysts, information specialists, or organizations are also facilitated by CDIAC`s staff. This report provides an account of the activities accomplished by CDIAC (including World Data Center-A for Atmospheric Trace Gases) during the period October 1, 1992, to September 30, 1993. An organizational overview of CDIAC and its staff is supplemented by a detailed description of inquiries received and CDIAC`s response to those inquiries. An analysis and description of the preparation and distribution of NDPS, CMPS, technical reports, newsletters, fact sheets, specialty publications, and reprints are provided. Comments and descriptions of CDIAC`s information management systems, professional networking, and special bilateral agreements are also presented.

  8. Carbon Dioxide Information Analysis Center: FY 1991 activities

    SciTech Connect (OSTI)

    Cushman, R.M.; Stoss, F.W.

    1992-06-01T23:59:59.000Z

    During the course of a fiscal year, Oak Ridge National Laboratory`s Carbon Dioxide Information Analysis Center (CDIAC) distributes thousands of specially publications-numeric data packages (NDPs), computer model packages (CMPs), technical reports, public communication publications, newsletters, article reprints, and reference books-in response to requests for information related to global environmental issues, primarily those pertaining to climate change. CDIAC`s staff also provides technical responses to specific inquiries related to carbon dioxide (CO{sub 2}), other trace gases, and climate. Hundreds of referrals to other researchers, policy analysts, information specialists, or organizations are also facilitated by CDIAC`s staff. This report provides an account of the activities accomplished by CDIAC during the period October 1, 1990 to September 30, 1991. An organizational overview of CDIAC and its staff is supplemented by a detailed description of inquiries received and CDIAC`s response to those inquiries. An analysis and description of the preparation and distribution of numeric data packages, computer model packages, technical reports, newsletters, factsheets, specially publications, and reprints is provided. Comments and descriptions of CDIAC`s information management systems, professional networking, and special bilateral agreements are also described.

  9. Chapter 1 Climate monitoring The European Commission strategy for global climate change studies and

    E-Print Network [OSTI]

    Daniel, Rosenfeld

    Chapter 1 Climate monitoring The European Commission strategy for global climate change studies, Jerusalem, Israel Precipitation as a centerpiece in Climate Change Water is the lifeblood of our livelihood on Earth. Temperature-driven inhabitable areas are due to too cold temperatures, and not due to excessively

  10. america surface temperature: Topics by E-print Network

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    of global climate sensitivity are explored in this work through the medium of Energy Balance Climate Models (EBCMs) and observational surface temperature data. In part...

  11. The Sun and Climate Solar Irradiance

    E-Print Network [OSTI]

    Walter, Frederick M.

    The Sun and Climate #12;Solar Irradiance The Solar Constant f = 1.4 x 106 erg/cm2/s. Over is higher when the Sun is more magnetically active. ·The Sun was magnetically active, and the climate the Sun Drive Climate? #12;The Temperature's Rising #12;Sunspots and CO2 What is Cause and What is Effect

  12. Climate change cripples forests October 1, 2012

    E-Print Network [OSTI]

    - 1 - Climate change cripples forests October 1, 2012 Southwestern US trees face rising drought, and several other partner organizations. 3:01 Tree Death Study's Climate Change Connection Described in a paper published in Nature Climate Change this week, "Temperature as a potent driver of regional forest

  13. Carbon Dioxide Information Analysis Center: FY 1992 activities

    SciTech Connect (OSTI)

    Cushman, R.M. [Oak Ridge National Lab., TN (United States). Carbon Dioxide Information Analysis Center; Stoss, F.W. [Tennessee Univ., Knoxville, TN (United States). Energy, Environment and Resources Center

    1993-03-01T23:59:59.000Z

    During the course of a fiscal year, Oak Ridge National Laboratory`s Carbon Dioxide Information Analysis Center (CDIAC) distributes thousands of specialty publications-numeric data packages (NDPs), computer model packages (CMPs), technical reports, public communication publications, newsletters, article reprints, and reference books-in response to requests for information related to global environmental issues, primarily those pertaining to climate change. CDIACs staff also provides technical responses to specific inquiries related to carbon dioxide (CO{sub 2}), other trace gases, and climate. Hundreds of referrals to other researchers, policy analysts, information specialists, or organizations are also facilitated by CDIAC`s staff. This report provides an account of the activities accomplished by CDIAC during the period October 1, 1991 to September 30, 1992. An organizational overview of CDIAC and its staff is supplemented by a detailed description of inquiries received and CDIAC`s response to those inquiries. As analysis and description of the preparation and distribution of numeric data packages, computer model packages, technical reports, newsletters, fact sheets, specialty publications, and reprints is provided. Comments and descriptions of CDIAC`s information management systems, professional networking, and special bilateral agreements are also described.

  14. RESEARCH ARTICLE High-resolution climate change mapping with gridded

    E-Print Network [OSTI]

    Vermont, University of

    RESEARCH ARTICLE High-resolution climate change mapping with gridded historical climate products of climate research and adaptation efforts around the world. High-resolution gridded historical climate (GHC products to produce high-resolution temperature trend maps for the US Northeast from 1980 to 2009

  15. Changing Climates 

    E-Print Network [OSTI]

    Wythe, Kathy

    2008-01-01T23:59:59.000Z

    and a wide range of academic areas are investigating the different compo- nents. More recently, they are taking information gleaned from the global climate models and applying them to research questions pertaining to Texas. Dr. Bruce Mc...Carl, Regents Professor of agricultural economics at Texas A&M University, has researched the economics of climate change for the last 20 years. McCarl, as a lead CHANGING CLIMATES tx H2O | pg. McCarl ] tx H2O | pg. 4 Changing Climates author...

  16. Essays on Agricultural Adaptation to Climate Change and Ethanol Market Integration in the U.S. 

    E-Print Network [OSTI]

    Aisabokhae, Ruth 1980-

    2012-12-05T23:59:59.000Z

    Climate factors like precipitation and temperature, being closely intertwined with agriculture, make a changing climate a big concern for the entire human race and its basic survival. Adaptation to climate is a long-running characteristic...

  17. The Impact of Climate Change on Electricity Demand in Thailand 

    E-Print Network [OSTI]

    Parkpoom, Suchao Jake

    2008-01-01T23:59:59.000Z

    Climate change is expected to lead to changes in ambient temperature, wind speed, humidity, precipitation and cloud cover. As electricity demand is closely influenced by these climatic variables, there is likely to be ...

  18. IMPACTS OF CLIMATE CHANGE ON SAN FRANCISCO BAY AREA

    E-Print Network [OSTI]

    IMPACTS OF CLIMATE CHANGE ON SAN FRANCISCO BAY AREA RESIDENTIAL ELECTRICITY CONSUMPTION anthropogenic climate change on residential electricity consumption for the nine San Francisco Bay Area counties with different meant temperatures on households' electricity consumption. The estimation uses a comprehensive

  19. Tree-ring reconstruction of maximum and minimum temperatures

    E-Print Network [OSTI]

    , minimum temperatures, diurnal temperature range, changing tree-ring/climate relationships, b; Vaganov et al. 1999; Bar- ber et al. 2000; Lloyd, Fastie 2002). Similar changes during investigations of tree- ring growth/climate relationships in interior British Columbia (BC

  20. What measures climate? A variety of variables including their variability and extreme values determine climate for

    E-Print Network [OSTI]

    Allan, Richard P.

    climate zones? The sun is the ultimate power source for the climate "machine". The uneven distribution conditions. Typical variables to consider are temperature (maximum, miniumum), precipitation (includes rain, sleet, snow, hail, etc), sunlight/cloudiness, wind, humidity, ice cover, sea temperature, etc... Many

  1. Climate Change and Forest Disturbances

    E-Print Network [OSTI]

    Dale, Virginia H.; Joyce, Linda A.; McNulty, Steve; Neilson, Ronald P.; Ayres, Matthew P.; Flannigan, Michael D.; Hanson, Paul J.; Irland, Lloyd C.; Lugo, Ariel E.; Peterson, Chris J.; Simberloff, Daniel; Swanson, Frederick J.; Stocks, Brian J.; Wotton, B. Michael; Peterson, A. Townsend

    2001-01-01T23:59:59.000Z

    of disturbances caused by climate change (e.g., Ojima et al. 1991).Yet modeling studies indicate the im- portance of climate effects on disturbance regimes (He et al. 1999). Local, regional, and global changes in temperature and precipitation can influence... circulation models (GCMs)—one de- veloped by the Hadley Center in the United Kingdom (HADCM2SUL) and one by the Canadian Climate Center (CGCM1)—have been selected for this national assessment (MacCracken et al. 2000). These transient GCMs simulate at...

  2. Climate Change and National Security

    SciTech Connect (OSTI)

    Malone, Elizabeth L.

    2013-02-01T23:59:59.000Z

    Climate change is increasingly recognized as having national security implications, which has prompted dialogue between the climate change and national security communities – with resultant advantages and differences. Climate change research has proven useful to the national security community sponsors in several ways. It has opened security discussions to consider climate as well as political factors in studies of the future. It has encouraged factoring in the stresses placed on societies by climate changes (of any kind) to help assess the potential for state stability. And it has shown that, changes such as increased heat, more intense storms, longer periods without rain, and earlier spring onset call for building climate resilience as part of building stability. For the climate change research community, studies from a national security point of view have revealed research lacunae, for example, such as the lack of usable migration studies. This has also pushed the research community to consider second- and third-order impacts of climate change, such as migration and state stability, which broadens discussion of future impacts beyond temperature increases, severe storms, and sea level rise; and affirms the importance of governance in responding to these changes. The increasing emphasis in climate change science toward research in vulnerability, resilience, and adaptation also frames what the intelligence and defense communities need to know, including where there are dependencies and weaknesses that may allow climate change impacts to result in security threats and where social and economic interventions can prevent climate change impacts and other stressors from resulting in social and political instability or collapse.

  3. Climate Engineering Responses to Climate Emergencies

    E-Print Network [OSTI]

    Battisti, David

    Novim Climate Engineering Responses to Climate Emergencies Jason J. Blackstock David S. Battisti Santa Barbara, California #12;Climate Engineering Responses to Climate Emergencies This report should, A. A. N. Patrinos, D. P. Schrag, R. H. Socolow and S. E. Koonin, Climate Engineering Responses

  4. DOI: 10.3334/CDIAC/vrc.ndp061 ORNL/CDIAC-107

    E-Print Network [OSTI]

    89512 Prepared by Robert M. Cushman Carbon Dioxide Information Analysis Center Environmental Sciences Office of Biological and Environmental Research Budget Activity Number KP 12 04 01 0 Prepared by the Carbon Dioxide Information Analysis Center OAK RIDGE NATIONAL LABORATORY Oak Ridge, Tennessee 37831

  5. Economic Damages from Climate Change: An Assessment of Market Impacts

    E-Print Network [OSTI]

    Hanemann, W Michael; Dale, Larry

    2006-01-01T23:59:59.000Z

    2: Projected Decrease in Water Equivalent of Sierra Snowpackof Averages Impacts on Water Sea Level Rise Temperature-Laboratory. Co-Director, Water Program, California Climate

  6. antarctic climate variability: Topics by E-print Network

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    ranges poleward. The endemic shelf fauna of Antarctica is especially vulnerable to climate-mediated biological invasions because cold temperatures currently exclude the...

  7. arm climate research: Topics by E-print Network

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    of Iron meteorites and confirm this prediction. We then check the hypothesis that climate, and in particular the temperature, is affected by the CRF to the extent that...

  8. alternative global climate: Topics by E-print Network

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Information Sciences Websites Summary: A Statistical Analysis of Global Inter-Annual Climate Anomalies in Monthly Sea Surface Temperature Records. Jian Huang and Finbarr...

  9. Multi-institutional project to study climate change's effect...

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    storage from the atmosphere (the carbon sink) may already be declining in response to climate change-induced reductions in precipitation and increases in temperature." Because...

  10. "Managing Department Climate Change"

    E-Print Network [OSTI]

    Sheridan, Jennifer

    "Managing Department Climate Change" #12;Presenters · Ronda Callister Professor, Department Department Climate? · Assesment is essential for determining strategies for initiating change · In a research climate · Each panelist will describe an intervention designed to improve department climate ­ Ronda

  11. Changing Climates

    E-Print Network [OSTI]

    Wythe, Kathy

    2008-01-01T23:59:59.000Z

    these data with predictions from the IPCC. Professor of geography at Texas State University, Dr. David Butler, does climate change research mainly in the Rocky Moun- tains with U.S. Geological Survey funding. He has also done research on how climate...://wiid.twdb.state.tx.us Detailed information about individual water wells. This system uses a geographic information system-based tool to show locations of water wells and download data on water levels and water quality. Reports that were developed about on-site conditions...

  12. Table of Contents Part 1: Climate Graphs Activity

    E-Print Network [OSTI]

    . Quantity. How much precipitation falls? What is the general trend east to west in Texas concerningTable of Contents Part 1: Climate Graphs Activity Part 2: Texas Climate Handout Maps for transparencies: a. Texas Average Annual Temperature b. Texas Average Annual Precipitation c. Texas Climate

  13. Climate Change and Human Health National Center for Environmental Health

    E-Print Network [OSTI]

    Climate Change and Human Health National Center for Environmental Health Division of Environmental and Prevention October 17, 2012 #12;Coastal flooding Climate change effects: ·Temperature ·Sea level,civil conflict Anxiety,despair,depression Civil conflict Climate Change Health Effects Food & water Malnutrition

  14. Mediterranean Seagrass Meadows: Resilience and Contribution to Climate Change Mitigation

    E-Print Network [OSTI]

    Boudouresque, Charles F.

    Mediterranean Seagrass Meadows: Resilience and Contribution to Climate Change Mitigation A Short to Climate Change Mitigation, A Short Summary / Les herbiers de Magnoliophytes marines de Méditerranée: 1 Evolution of the average temperature and level of the sea since 1850 (after Climate Change 2007

  15. Climate Forcings and Climate Sensitivities Diagnosed from Coupled Climate Model Integrations

    SciTech Connect (OSTI)

    Forster, P M A F; Taylor, K E

    2006-07-25T23:59:59.000Z

    A simple technique is proposed for calculating global mean climate forcing from transient integrations of coupled Atmosphere Ocean General Circulation Models (AOGCMs). This 'climate forcing' differs from the conventionally defined radiative forcing as it includes semi-direct effects that account for certain short timescale responses in the troposphere. Firstly, we calculate a climate feedback term from reported values of 2 x CO{sub 2} radiative forcing and surface temperature time series from 70-year simulations by twenty AOGCMs. In these simulations carbon dioxide is increased by 1%/year. The derived climate feedback agrees well with values that we diagnose from equilibrium climate change experiments of slab-ocean versions of the same models. These climate feedback terms are associated with the fast, quasi-linear response of lapse rate, clouds, water vapor and albedo to global surface temperature changes. The importance of the feedbacks is gauged by their impact on the radiative fluxes at the top of the atmosphere. We find partial compensation between longwave and shortwave feedback terms that lessens the inter-model differences in the equilibrium climate sensitivity. There is also some indication that the AOGCMs overestimate the strength of the positive longwave feedback. These feedback terms are then used to infer the shortwave and longwave time series of climate forcing in 20th and 21st Century simulations in the AOGCMs. We validate the technique using conventionally calculated forcing time series from four AOGCMs. In these AOGCMs the shortwave and longwave climate forcings we diagnose agree with the conventional forcing time series within {approx}10%. The shortwave forcing time series exhibit order of magnitude variations between the AOGCMs, differences likely related to how both natural forcings and/or anthropogenic aerosol effects are included. There are also factor of two differences in the longwave climate forcing time series, which may indicate problems with the modeling of well-mixed-greenhouse-gas changes. The simple diagnoses we present provide an important and useful first step for understanding differences in AOGCM integrations, indicating that some of the differences in model projections can be attributed to different prescribed climate forcing, even for so-called standard climate change scenarios.

  16. Regional climate model data used within the SWURVE project 2: addressing uncertainty in regional climate model data Hydrol. Earth Syst. Sci., 11(1), 10851096, 2007

    E-Print Network [OSTI]

    Boyer, Edmond

    .Ekstrom@uea.ac.uk Abstract To aid assessments of the impact of climate change on water related activities in the case study on the impacts of climate change on specific water management activities (Kilsby, 2007). Uncertainties linked, temperature, rainfall, Europe Introduction As climate model projections are often used in climate change

  17. Predicting future climate change for the UK and East AngliaPredicting future climate change for the UK and East Anglia Climatic Research Unit (CRU), University of East Anglia, Norwich

    E-Print Network [OSTI]

    Feigon, Brooke

    Predicting future climate change for the UK and East AngliaPredicting future climate change confidence in the following future changes in UK climate: Average temperature increases Summer temperature part in farming, so we might expect these changes to have an impact on agriculture ­ affecting both

  18. Surface temperature trends in Russia over the past five centuries reconstructed from borehole temperatures

    E-Print Network [OSTI]

    Smerdon, Jason E.

    ; KEYWORDS: Russia, borehole temperatures, climate reconstruction Citation: Pollack, H. N., D. Y. Demezhko, A and extent of 20th century temperature changes in Russia, within the context of the temperature history of climate changing on decadal, centennial, or millennial timescales, the outward flux and its subsurface

  19. 1, 255285, 2005 Extreme climates

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    , orography, and oceanic heat transport on extreme climates V. Romanova 1 , G. Lohmann 2,1 , and K. Grosfeld 2 to assess the possibility that land albedo, atmospheric CO2, orography and oceanic heat transport may cause5-covered Earth is the high land albedo in combination with initial temperatures set equal to the freezing point

  20. Colorado Climate Update Nolan Doesken

    E-Print Network [OSTI]

    to the Colorado Farm Show Wednesday, January 30, 2013 Prepared by Wendy Ryan and Zach Schwalbe #12;Topics we;Monitoring our Climate · Elements: temperature, precipitation, snow, wind, solar, evaporation, soil Average Solar Radiation National Renewal Energy Laboratory: www.nrel.gov Colorado is a part

  1. Climate Change, Adaptation, and Development

    E-Print Network [OSTI]

    Cole, Daniel H.

    2008-01-01T23:59:59.000Z

    Climate Change, Adaptation, and Development Daniel H. Cole*THE COSTS OF CLIMATE CHANGE . ADAPTATIONCONVENTION ON CLIMATE CHANGE . IV. A.

  2. Sandia National Laboratories: Climate Security

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    MonitoringClimate Security Climate Security Climate Security Global reductions in greenhouse gases will eventually be motivated by an international climate treaty and will entail...

  3. A climatic thermostat making Earth habitable

    E-Print Network [OSTI]

    Peter D. Ditlevsen

    2005-05-12T23:59:59.000Z

    The mean surface temperature on Earth and other planets with atmospheres is determined by the radiative balance between the non-reflected incoming solar radiation and the outgoing long-wave black-body radiation from the atmosphere. The surface temperature is higher than the black-body temperature due to the greenhouse warming. Balancing the ice-albedo cooling and the greenhouse warming gives rise to two stable climate states. A cold climate state with a completelyice-covered planet, called Snowball Earth, and a warm state similar to our present climate where greenhouse warming prevents the total glacition. The warm state has dominated Earth in most of its geological history despite a 30 % fainter young Sun. The warming could have been controlled by a greenhouse thermostat operating by temperature control of the weathering process depleting the atmosphere from $CO_2$. This temperature control has permitted life to evolve as early as the end of the heavy bombartment 4 billion years ago.

  4. Climate change

    ScienceCinema (OSTI)

    Iversen, Colleen

    2014-05-23T23:59:59.000Z

    Ecologist Colleen Iversen uses field study in Minnesota and Alaska to understand how increased atmospheric carbon dioxide and warmer temperatures affect plant growth.

  5. Climate change

    SciTech Connect (OSTI)

    Iversen, Colleen

    2014-05-02T23:59:59.000Z

    Ecologist Colleen Iversen uses field study in Minnesota and Alaska to understand how increased atmospheric carbon dioxide and warmer temperatures affect plant growth.

  6. Climate Change Scoping Plan

    E-Print Network [OSTI]

    Climate Change Scoping Plan a amework for change Prepared by the California Air Resources BoardBackgroundBackgroundBackground ............................................................................................................................................................................................................................................................................................................................................................................................................ 4444 1. Climate Change Policy in California1. Climate Change Policy in California1. Climate Change Policy in California1. Climate Change Policy in California

  7. Climate Change Scoping Plan

    E-Print Network [OSTI]

    Climate Change Scoping Plan a amework for change as approved Prepared by the California AirBackgroundBackgroundBackground ............................................................................................................................................................................................................................................................................................................................................................................................................ 4444 1. Climate Change Policy in California1. Climate Change Policy in California1. Climate Change Policy in California1. Climate Change Policy in California

  8. Climate change action plan

    E-Print Network [OSTI]

    Delivery Climate change action plan 2009-2011 #12;2 | Climate change action plan ©istockphoto.com #12;Climate Change Action Plan Climate change action plan | 3 Contents Overview 4 Preface and Introduction 5 Climate change predictions for Scotland 6 The role of forestry 7 Protecting and managing

  9. Information theory and climate prediction

    E-Print Network [OSTI]

    Leung, Lai-yung

    1988-01-01T23:59:59.000Z

    as different as two states chosen at random (Lorenz, 1969b). ln this research, we are concerned with the prediction of climate in which there is no change of external forcing. Lorenz (1975) referred to this case as the predictability of the first kind... used as such a quantity (e. g. Barnett and Hasselmann, 1979). Time Figure 1. A Subensemble of Systems that Pass Through the Neighborhood of Initial Temperature Anomaly To The signal is the change of some climatic variable which we want to predict...

  10. Policy-relevant science to help solve the carbon-climate problem

    E-Print Network [OSTI]

    2009 #12;#12;Carbon emissions and the scale of the problem #12;#12;Rates of atmospheric CO2 change Calculated from Petit et al (1999) Calculated from Keeling and Whorf (2005) #12;Anthropogenic CO2 emissions et al. 2007, PNAS 1990 1995 2000 2005 2010 CO2Emissions(GtCy-1 ) 5 6 7 8 9 10 Actual emissions: CDIAC

  11. Climate Past, Climate Present, Climate Future Douglas Nychka,

    E-Print Network [OSTI]

    Nychka, Douglas

    series and an energy balance model. 1000 1200 1400 1600 1800 2000 -1.5-1.0-0.50.00.5 Year Degree. Supported by US NSF 7th World Congress Prob. and Stat., Singapore July 2008 #12;What is climate? Climate will use statistics to talk about the "known un- knowns" for the Earth's climate Statistics uses

  12. Climatic effects of 1950–2050 changes in US anthropogenic aerosols – Part 2: Climate response

    E-Print Network [OSTI]

    Leibensperger, Eric Michael

    We investigate the climate response to changing US anthropogenic aerosol sources over the 1950–2050 period by using the NASA GISS general circulation model (GCM) and comparing to observed US temperature trends. Time-dependent ...

  13. Climate Action Plan (Delaware)

    Broader source: Energy.gov [DOE]

    To better understand the current and future vulnerabilities and risks to climate change, DNREC Secretary Collin O’Mara directed the Division of Energy and Climate to conduct a statewide climate...

  14. Climate Data Operators (CDO)

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Climate Data Operators (CDO) Climate Data Operators (CDO) Description and Overview CDO is a large tool set for working on climate data. NetCDF 34, GRIB including SZIP compression,...

  15. Protecting climate with forests.

    E-Print Network [OSTI]

    2008-01-01T23:59:59.000Z

    Changing feedbacks in the climate–biosphere system Front.313–32 Bonan G B 2008 Forests and climate change: forcings,feedbacks, and the climate benefits of forests Science

  16. Climate Code Foundation

    E-Print Network [OSTI]

    Barnes, Nick; Jones, David

    2011-07-05T23:59:59.000Z

    Climate Code Foundation - who are we? A non-profit organisation founded in August 2010; our goal is to promote the public understanding of climate science, by increasing the visibility and clarity of the software used in climate science...

  17. Energy Piles in Cooling Dominated Climates

    E-Print Network [OSTI]

    Akrouch, Ghassan

    2014-04-10T23:59:59.000Z

    . In summer, ground temperature is lower than air temperature, and so the ground may be used as a heat sink. The opposite is true in winter; the ground becomes a heat source. This technology is used efficiently in cold, heating dominated climates. Could...

  18. IEA HPP Annex 41 Cold Climate Heat

    E-Print Network [OSTI]

    Oak Ridge National Laboratory

    of Air-Source Heat Pumps Van D. Baxter Oak Ridge National Laboratory European Heat Pump Summit Nuremberg ­ Cold Climate Heat Pumps Improving low ambient temperature performance of air-source heat pumps as having large number of hours with OD temperature -7 °C (19 °F). Air-source heat pumps (ASHP

  19. Climate VISION: Contact Us

    Office of Scientific and Technical Information (OSTI)

    of Energy Office of Climate Change Policy and Technology (PI-50) 202-586-8339 Mining - Contacts Association Climate VISION Lead Constance Holmes Senior Economist, Director...

  20. Sandia National Laboratories: Climate

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Climate A Model for the Nation: Promoting Education and Innovation in Vermont's Electricity Sector On May 8, 2012, in Climate, Customers & Partners, Energy, Energy Surety,...

  1. Climate Action Plan (Montana)

    Broader source: Energy.gov [DOE]

    Recognizing the profound implications that global warming and climate variation could have on the economy, environment and quality of life in Montana, the Climate Change Advisory Committee (CCAC)...

  2. Climate change cripples forests

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Climate change cripples forests Climate change cripples forests A team of scientists concluded that in the warmer and drier Southwest of the near future, widespread tree mortality...

  3. Climate change cripples forests

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Climate Change Cripples Forests Climate change cripples forests A team of scientists concluded that in the warmer and drier Southwest of the near future, widespread tree mortality...

  4. Climate Change Response

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    the Interior Climate Change Response "From the Everglades to the Great Lakes to Alaska and everywhere in between, climate change is a leading threat to natural and cultural...

  5. On the origins of the ice ages : insolation forcing, age models, and nonlinear climate change

    E-Print Network [OSTI]

    Huybers, Peter, 1974-

    2004-01-01T23:59:59.000Z

    This thesis revolves about the relationship between orbital forcing and climate variability. To place paleo and modern climate variability in context, the spectrum of temperature variability is estimated from time-scales ...

  6. Climate change, mortality, and adaptation : evidence from annual fluctuations in weather in the US

    E-Print Network [OSTI]

    Deschênes, Olivier

    2007-01-01T23:59:59.000Z

    This paper produces the first large-scale estimates of the US health related welfare costs due to climate change. Using the presumably random year-to-year variation in temperature and two state of the art climate models, ...

  7. Climate Leadership Conference

    Broader source: Energy.gov [DOE]

    Hosted and organized by the Association of Climate Change Officers (ACCO), Center for Climate and Energy Solutions (C2ES), and the Climate Registry, the three-day conference will showcase how new business opportunities, current policies, technologies, climate solutions and energy transformation will drive our low-carbon future.

  8. programs in climate change

    E-Print Network [OSTI]

    existing programs in climate change science and infrastructure. The Laboratory has a 15- year history in climate change science. The Climate, Ocean and Sea Ice Modeling (COSIM) project develops and maintains advanced numerical models of the ocean, sea ice, and ice sheets for use in global climate change

  9. Detection of CO/sub 2/-induced climate change. Progress report, 1 December 1985-15 July 1986

    SciTech Connect (OSTI)

    Wigley, T.M.L.; Jones, P.D.

    1986-07-15T23:59:59.000Z

    The objective is to assemble and analyze present and past instrumental climate data as a basis for detecting CO/sub 2/-induced climatic change and for validation of climate models. This report describes progress in the following areas: (1) southern hemisphere temperature data; (2) updating of gridded temperature data; (3) satellite data; (4) marine temperature data sets; (5) analysis of gridded mean sea level pressure data; (6) regional validation of climate models; and (7) detection studies. (ACR)

  10. Formulating Climate Change Scenarios to Inform Climate - Resilient...

    Open Energy Info (EERE)

    Formulating Climate Change Scenarios to Inform Climate - Resilient Development Strategies Jump to: navigation, search Tool Summary LAUNCH TOOL Name: Formulating Climate Change...

  11. Global Climate Change Impacts:Global Climate Change Impacts: Implications for Climate EngineeringImplications for Climate Engineering

    E-Print Network [OSTI]

    Polz, Martin

    Global Climate Change Impacts:Global Climate Change Impacts: Implications for Climate Engineering Center Global Climate Change Impacts in the United States October 29, 2009 #12;2Global Climate Change Impacts in the United States 2 Response Strategies to ClimateResponse Strategies to Climate ChangeChange

  12. Time varying arctic climate change amplification

    SciTech Connect (OSTI)

    Chylek, Petr [Los Alamos National Laboratory; Dubey, Manvendra K [Los Alamos National Laboratory; Lesins, Glen [DALLHOUSIE U; Wang, Muyin [NOAA/JISAO

    2009-01-01T23:59:59.000Z

    During the past 130 years the global mean surface air temperature has risen by about 0.75 K. Due to feedbacks -- including the snow/ice albedo feedback -- the warming in the Arctic is expected to proceed at a faster rate than the global average. Climate model simulations suggest that this Arctic amplification produces warming that is two to three times larger than the global mean. Understanding the Arctic amplification is essential for projections of future Arctic climate including sea ice extent and melting of the Greenland ice sheet. We use the temperature records from the Arctic stations to show that (a) the Arctic amplification is larger at latitudes above 700 N compared to those within 64-70oN belt, and that, surprisingly; (b) the ratio of the Arctic to global rate of temperature change is not constant but varies on the decadal timescale. This time dependence will affect future projections of climate changes in the Arctic.

  13. air temperature variations: Topics by E-print Network

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    appears to be driven by seasonal variations in the total aboveground biomass of the treatment wetland. We found that only air temperature and PAR were significant climatic...

  14. Climate change risk and response

    E-Print Network [OSTI]

    Kahrl, Fredrich; Roland-Holst, David

    2008-01-01T23:59:59.000Z

    the Potential Consequences of Climate Variability and Changeand Kate Scow. 2006. “Climate Change: Page 117 ChallengesLandscapes. ” California Climate Change Center White Paper.

  15. Climate change risk and response

    E-Print Network [OSTI]

    Kahrl, Fredrich; Roland-Holst, David

    2008-01-01T23:59:59.000Z

    and Kate Scow. 2006. “Climate Change: Page 117 ChallengesLandscapes. ” California Climate Change Center White Paper.Sea Level. ” California Climate Change Center White Paper.

  16. Climate Change and National Security

    E-Print Network [OSTI]

    Alyson, Fleming; Summer, Kelly; Summer, Martin; Lauren, Franck; Jonathan, Mark

    2015-01-01T23:59:59.000Z

    CLIMATE CHANGE Multiplying Threats to National Securityfor the impacts of climate change on national security. Pagea warming world. Page 11 “Climate change acts as a threat

  17. Climate change risk and response

    E-Print Network [OSTI]

    Kahrl, Fredrich; Roland-Holst, David

    2008-01-01T23:59:59.000Z

    net impact of climate change on agriculture in California,of Climate Change on California Agriculture. ” PresentationEffects of Climate Change on California Agriculture Positive

  18. Climate Change and Agriculture Reconsidered

    E-Print Network [OSTI]

    Fisher, Anthony

    2009-01-01T23:59:59.000Z

    2009 Paper 1080 Climate Change and Agriculture Reconsideredby author(s). Climate Change and Agriculture Reconsideredimpact of climate change on agriculture, there still exists

  19. Developing Models for Predictive Climate Science

    SciTech Connect (OSTI)

    Drake, John B [ORNL; Jones, Philip W [Los Alamos National Laboratory (LANL)

    2007-01-01T23:59:59.000Z

    The Community Climate System Model results from a multi-agency collaboration designed to construct cutting-edge climate science simulation models for a broad research community. Predictive climate simulations are currently being prepared for the petascale computers of the near future. Modeling capabilities are continuously being improved in order to provide better answers to critical questions about Earth's climate. Climate change and its implications are front page news in today's world. Could global warming be responsible for the July 2006 heat waves in Europe and the United States? Should more resources be devoted to preparing for an increase in the frequency of strong tropical storms and hurricanes like Katrina? Will coastal cities be flooded due to a rise in sea level? The National Climatic Data Center (NCDC), which archives all weather data for the nation, reports that global surface temperatures have increased over the last century, and that the rate of increase is three times greater since 1976. Will temperatures continue to climb at this rate, will they decline again, or will the rate of increase become even steeper? To address such a flurry of questions, scientists must adopt a systematic approach and develop a predictive framework. With responsibility for advising on energy and technology strategies, the DOE is dedicated to advancing climate research in order to elucidate the causes of climate change, including the role of carbon loading from fossil fuel use. Thus, climate science--which by nature involves advanced computing technology and methods--has been the focus of a number of DOE's SciDAC research projects. Dr. John Drake (ORNL) and Dr. Philip Jones (LANL) served as principal investigators on the SciDAC project, 'Collaborative Design and Development of the Community Climate System Model for Terascale Computers.' The Community Climate System Model (CCSM) is a fully-coupled global system that provides state-of-the-art computer simulations of the Earth's past, present, and future climate states. The collaborative SciDAC team--including over a dozen researchers at institutions around the country--developed, validated, documented, and optimized the performance of CCSM using the latest software engineering approaches, computational technology, and scientific knowledge. Many of the factors that must be accounted for in a comprehensive model of the climate system are illustrated in figure 1.

  20. Climate ChangeClimate Change and Runoff Managementand Runoff Management

    E-Print Network [OSTI]

    Sheridan, Jennifer

    Climate ChangeClimate Change and Runoff Managementand Runoff Management in Wisconsinin Wisconsin NASECA February 3, 2011 David S. Liebl #12;Overview · Understanding climate change · Wisconsin's changing climate · Expected impacts · Adaptation strategies #12;Visible Light Energy in = Energy out Absorbed

  1. PhotoYannArthus-Bertrand/Altitude CLIMATE CHANGE 2013

    E-Print Network [OSTI]

    Photo©YannArthus-Bertrand/Altitude CLIMATE CHANGE 2013 The Physical Science Basis WGI Technical). Observational and model studies of temperature change, climate feedbacks and changes in the Earth's energy in warming of the atmosphere and the ocean, in changes in the global water cycle, in reductions in snow

  2. Minimizing Irreversible Impacts of Human-Made Climate Change

    E-Print Network [OSTI]

    Hansen, James E.

    Geophysical Union San Francisco, CA #12;Climate Impacts 1. Ice Sheet Disintegration & Sea Level - Ocean Warming Ice Shelves Melt Ice Streams Surge Disintegration 2. Species Extermination - Shifting Climate-25 meters - Pliocene temperature +3-4°C* Ice sheet response time uncertain, but it is shorter than

  3. Hot climates, high sensitivity R. T. Pierrehumbert1

    E-Print Network [OSTI]

    Pierrehumbert, Raymond

    the energy bud- get back into balance. Climate sensitivity is determined by the relative slopes of the two Humidity Clear State Energyfluxintooroutofplanet Surface Temperature Solar energy in Infrared out, low CO2. Schematic of the way the Earth's energy budget introduces state-dependent climate sensitivity in ref. 2

  4. Global warming and Arctic climate. Raymond S. Bradley

    E-Print Network [OSTI]

    Mountziaris, T. J.

    Global warming and Arctic climate. Raymond S. Bradley Climate System Research Center University of Massachusetts Amherst #12;How have global temperatures changed & why? 1. Average instrumental records from around the world; express all as anomalies from 1961-90 average #12;#12;Overall trend is upward ("global

  5. Climate WorkshopsClimate Workshops for Department Chairsp

    E-Print Network [OSTI]

    Tilbury, Dawn

    Climate WorkshopsClimate Workshops for Department Chairsp University of Wisconsin ADVANCE-IT Slides) #12;Why focus on departmental climate? Individuals experience climate in their immediate workplace negative climate than male faculty Improving department climate is critical for retention and advancement

  6. Climate Leadership Conference

    Office of Energy Efficiency and Renewable Energy (EERE)

    The Climate Leadership Conference is your annual exchange for addressing global climate change through policy, innovation, and business solutions. Forward-thinking lead­ers from busi­ness, gov­ern...

  7. The Climate Policy Dilemma

    E-Print Network [OSTI]

    Pindyck, Robert S.

    Climate policy poses a dilemma for environmental economists. The economic argument for stringent GHG abatement is far from clear. There is disagreement among both climate scientists and economists over the likelihood of ...

  8. Sandia National Laboratories: Climate

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    to address the most challenging and demanding climate-change issues. Accelerated Climate Modeling for Energy (ACME) is designed to accel-erate the development and applica-tion of...

  9. The Climate Policy Dilemma

    E-Print Network [OSTI]

    Pindyck, Robert S.

    Climate policy poses a dilemma for environmental economists. The economic argument for stringent greenhouse gas (GHG) abatement is far from clear. There is disagreement among both climate scientists and economists concerning ...

  10. Extracting a Climate Signal from 169 Glacier Records

    E-Print Network [OSTI]

    Wright, Dawn Jeannine

    Extracting a Climate Signal from 169 Glacier Records J. Oerlemans I constructed a temperature history for different parts of the world from 169 glacier length records. Using a first-order theory of glacier dynamics, I related changes in glacier length to changes in temperature. The derived temperature

  11. Climate Change Economics and Policy

    E-Print Network [OSTI]

    Romano, Daniela

    AFRICA COLLEGE Centre for Climate Change Economics and Policy Adapting to Climate Change 3 CLIMATE...Furthermore, there is strong scientific evidence that climate change will disrupt the global economy, environment and society a growing population in a changing climate is, therefore, a major global challenge. Changes in climate

  12. Fat Tails, Thin Tails, and Climate Change Policy

    E-Print Network [OSTI]

    Pindyck, Robert S.

    2012-01-01T23:59:59.000Z

    Climate policy is complicated by the considerable uncertainties concerning the benefits and costs of abatement. We do not even know the probability distributions for future temperatures and impacts, making benefit–cost ...

  13. Evaluation of Energy Efficiency Measures in Hot and Humid Climates

    E-Print Network [OSTI]

    Zhao, Y.; Erwine, B.; Leonard, P.; Pease, B.; Dole, A.; Lee, A.

    Hot and humid climates present some of the most complex challenges for sustainable building designs. High temperatures coupled with high humidity create extreme comfort problems and exacerbate the potential for condensation, mold and mildew...

  14. The Climate Policy Narrative for a Dangerously Warming World

    SciTech Connect (OSTI)

    Sanford, Todd [Union of Concerned Scientists] [Union of Concerned Scientists; Frumhoff, Peter [Union of Concerned Scientists] [Union of Concerned Scientists; Luers, Amy [Skoll Global Threats Fund] [Skoll Global Threats Fund; Gulledge, Jay [ORNL] [ORNL

    2014-01-01T23:59:59.000Z

    It is time to acknowledge that global average temperatures will likely rise above the 2 C policy target and consider how that deeply troubling prospect should affect priorities for communicating and managing the risks of a dangerously warming climate.

  15. Fat Tails, Thin Tails, and Climate Change Policy

    E-Print Network [OSTI]

    Pindyck, Robert S.

    Climate policy is complicated by the considerable compounded uncertainties over the costs and benefits of abatement. We don’t even know the probability distributions for future temperatures and impacts, making cost-benefit ...

  16. Campus Conversations: CLIMATE CHANGE

    E-Print Network [OSTI]

    Attari, Shahzeen Z.

    booklet is an adaptation and updating of Global Warming and Climate Change, a brochure developed in 1994 that will address climate change. Scientists tell us that the climate of the earth is warming, and that the warming into the foundation of the world economy and into the everyday things we do (driving) and use (electricity). Thus

  17. METEOROLOGICAL Journal of Climate

    E-Print Network [OSTI]

    Feng, Ming

    AMERICAN METEOROLOGICAL SOCIETY Journal of Climate EARLY ONLINE RELEASE This is a preliminary PDF it is available. © 201 American Meteorological Society1 #12;Sun et al. climate downscaling of the Australian currents 1 Marine downscaling of a future climate scenario for Australian boundary currents Chaojiao Sun

  18. Campus Climate Camden Campus

    E-Print Network [OSTI]

    Hanson, Stephen José

    Campus Climate Report Camden Campus New Brunswick/Piscataway Campus Newark Campus Student Survey #12;I. INTRODUCTION Executive Summary The Rutgers Campus Climate Survey was designed to determine how University, the campus climate surveys revealed strong areas of satisfaction with the Rutgers University

  19. Forest Research: Climate Change

    E-Print Network [OSTI]

    Forest Research: Climate Change projects Forest Research is part of the Forestry Commission of climate change-related research is wide-ranging, covering impact assessment and monitoring, adaptation around a quarter of its research budget with Forest Research on climate change and related programmes

  20. Climate Change Workshop 2007

    E-Print Network [OSTI]

    Nebraska-Lincoln, University of

    1 Climate Change Workshop 2007 Adaptive Management and Resilience Relevant for the Platte River, UNL Climate Change Workshop 2007 · Resilience ·Why it matters · Adaptive Management ·How it helps ·Adaptive Capacity · What it is Overview Climate Change Workshop 2007 "A public Domain, once a velvet carpet

  1. Climate Change Projections of the North American Regional Climate Change Assessment Program (NARCCAP)

    SciTech Connect (OSTI)

    Mearns, L. O.; Sain, Steve; Leung, Lai-Yung R.; Bukovsky, M. S.; McGinnis, Seth; Biner, S.; Caya, Daniel; Arritt, R.; Gutowski, William; Takle, Eugene S.; Snyder, Mark A.; Jones, Richard; Nunes, A M B.; Tucker, S.; Herzmann, D.; McDaniel, Larry; Sloan, Lisa

    2013-10-01T23:59:59.000Z

    We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated climate changes differ from those of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation: larger increases in the northern part of the domain in winter and greater decreases across a swath of the central part in summer, compared to the four GCMs driving the regional models as well as to the full set of CMIP3 GCM results. We pose some possible process-level mechanisms for the difference in intensity of change, particularly for summer. Detailed process-level studies will be necessary to establish mechanisms and credibility of these results. The GCMs explain more variance for winter temperature and the RCMs for summer temperature. The same is true for precipitation patterns. Thus, we recommend that future RCM-GCM experiments over this region include a balanced number of GCMs and RCMs.

  2. Carbon Dioxide Information Analysis Center: FY 1991 activities

    SciTech Connect (OSTI)

    Cushman, R.M.; Stoss, F.W.

    1992-06-01T23:59:59.000Z

    During the course of a fiscal year, Oak Ridge National Laboratory's Carbon Dioxide Information Analysis Center (CDIAC) distributes thousands of specially publications-numeric data packages (NDPs), computer model packages (CMPs), technical reports, public communication publications, newsletters, article reprints, and reference books-in response to requests for information related to global environmental issues, primarily those pertaining to climate change. CDIAC's staff also provides technical responses to specific inquiries related to carbon dioxide (CO{sub 2}), other trace gases, and climate. Hundreds of referrals to other researchers, policy analysts, information specialists, or organizations are also facilitated by CDIAC's staff. This report provides an account of the activities accomplished by CDIAC during the period October 1, 1990 to September 30, 1991. An organizational overview of CDIAC and its staff is supplemented by a detailed description of inquiries received and CDIAC's response to those inquiries. An analysis and description of the preparation and distribution of numeric data packages, computer model packages, technical reports, newsletters, factsheets, specially publications, and reprints is provided. Comments and descriptions of CDIAC's information management systems, professional networking, and special bilateral agreements are also described.

  3. Climate Variability and Climate Change: The New Climate Dice 10 November 2011

    E-Print Network [OSTI]

    Hansen, James E.

    1 Climate Variability and Climate Change: The New Climate Dice 10 November 2011 J. Hansen, M. Sato, coincident with increased global warming. The most dramatic and important change of the climate dice change is the natural variability of climate. How can a person discern long-term climate change, given

  4. Sunlight, Clouds, and Climate Charlie Zender

    E-Print Network [OSTI]

    Zender, Charles

    of temperature, rainfall, wind... ­ Averages taken over 1000's of miles, many years ­ Climate is intrinsically" = "Radiation" = "Light" = "Photons" ­ Photons are Light travel at the speed of light ­ Photons travel like (Axial tilt): 41 ka cycle ­ Angle of inclination cycles from 22.1­24.5 ­ Angle is 23.5 now

  5. Extremes in climate science Andreas Sterl (KNMI)

    E-Print Network [OSTI]

    Stoffelen, Ad

    (non-deterministic) influences: sun, volcanoes, anthropogenic effects (GHG emissions) => deterministic Sterl, PhysMathClim Climate change GHG concentrations increase => Temperature increases => other weather;31.01.2012, Utrecht Andreas Sterl, PhysMathClim EVT - 1 Extremes: tail of a distribution => few observations => tail

  6. Perception of climate change James Hansena,1

    E-Print Network [OSTI]

    Kammen, Daniel M.

    the significance of human- made global warming. Actions to stem emissions of the gases that cause global warming the season when climate change will have its biggest impact on humanity. Global warming causes spring warmth global warming. The distribution of seasonal mean temperature anomalies has shifted toward higher tempera

  7. Uncertainty in Simulating Wheat Yields Under Climate Change

    SciTech Connect (OSTI)

    Asseng, S.; Ewert, F.; Rosenzweig, C.; Jones, J.W.; Hatfield, Jerry; Ruane, Alex; Boote, K. J.; Thorburn, Peter; Rotter, R.P.; Cammarano, D.; Brisson, N.; Basso, B.; Martre, P.; Aggarwal, P.K.; Angulo, C.; Bertuzzi, P.; Biernath, C.; Challinor, AJ; Doltra, J.; Gayler, S.; Goldberg, R.; Grant, Robert; Heng, L.; Hooker, J.; Hunt, L.A.; Ingwersen, J.; Izaurralde, Roberto C.; Kersebaum, K.C.; Mueller, C.; Naresh Kumar, S.; Nendel, C.; O'Leary, G.O.; Olesen, JE; Osborne, T.; Palosuo, T.; Priesack, E.; Ripoche, D.; Semenov, M.A.; Shcherbak, I.; Steduto, P.; Stockle, Claudio O.; Stratonovitch, P.; Streck, T.; Supit, I.; Tao, F.; Travasso, M.; Waha, K.; Wallach, D.; White, J.W.; Williams, J.R.; Wolf, J.

    2013-09-01T23:59:59.000Z

    Anticipating the impacts of climate change on crop yields is critical for assessing future food security. Process-based crop simulation models are the most commonly used tools in such assessments1,2. Analysis of uncertainties in future greenhouse gas emissions and their impacts on future climate change has been increasingly described in the literature3,4 while assessments of the uncertainty in crop responses to climate change are very rare. Systematic and objective comparisons across impact studies is difficult, and thus has not been fully realized5. Here we present the largest coordinated and standardized crop model intercomparison for climate change impacts on wheat production to date. We found that several individual crop models are able to reproduce measured grain yields under current diverse environments, particularly if sufficient details are provided to execute them. However, simulated climate change impacts can vary across models due to differences in model structures and algorithms. The crop-model component of uncertainty in climate change impact assessments was considerably larger than the climate-model component from Global Climate Models (GCMs). Model responses to high temperatures and temperature-by-CO2 interactions are identified as major sources of simulated impact uncertainties. Significant reductions in impact uncertainties through model improvements in these areas and improved quantification of uncertainty through multi-model ensembles are urgently needed for a more reliable translation of climate change scenarios into agricultural impacts in order to develop adaptation strategies and aid policymaking.

  8. The Antarctic climate anomaly and galactic cosmic rays

    E-Print Network [OSTI]

    Svensmark, H

    2006-01-01T23:59:59.000Z

    It has been proposed that galactic cosmic rays may influence the Earth's climate by affecting cloud formation. If changes in cloudiness play a part in climate change, their effect changes sign in Antarctica. Satellite data from the Earth Radiation Budget Experiment (ERBE) are here used to calculate the changes in surface temperatures at all latitudes, due to small percentage changes in cloudiness. The results match the observed contrasts in temperature changes, globally and in Antarctica. Evidently clouds do not just respond passively to climate changes but take an active part in the forcing, in accordance with changes in the solar magnetic field that vary the cosmic-ray flux.

  9. Near-Term Climate Mitigation by Short-Lived Forcers

    SciTech Connect (OSTI)

    Smith, Steven J.; Mizrahi, Andrew H.

    2013-08-12T23:59:59.000Z

    Emissions reductions focused on anthropogenic climate forcing agents with relatively short atmospheric lifetimes such as methane (CH4) and black carbon (BC) have been suggested as a strategy to reduce the rate of climate change over the next several decades. We find that reductions of methane and BC would likely have only a modest impact on near-term climate warming. Even with maximally feasible reductions phased in from 2015 to 2035, global mean temperatures in 2050 are reduced by 0.16 °C, with an uncertainty range of 0.04-0.36°C, with the high end of this range only possible if total historical aerosol forcing is small. More realistic mitigation scenarios would likely provide a smaller climate benefit. The climate benefits from targeted reductions in short-lived forcing agents are smaller than previously estimated and are not substantially different in magnitude from the benefits due to a comprehensive climate policy.

  10. Is this climate porn? How does climate change communication

    E-Print Network [OSTI]

    Watson, Andrew

    Is this climate porn? How does climate change communication affect our perceptions and behaviour;1 Is this climate porn? How does climate change communication affect our perceptions and behaviour? Thomas D. Lowe 1 these kinds of messages (which have recently been dubbed `climate porn' (Ereaut and Segnit, 2006)), can

  11. Climate history and paleoclimate -HS 2011 Climate proxies

    E-Print Network [OSTI]

    Gilli, Adrian

    Climate history and paleoclimate - HS 2011 Climate proxies 18O Climate History & Paleoclimate ­ September 30, 2011 #12;How do we know about the past? Instrumental Historical Through proxies Climate proxies Climate history and paleoclimate - HS 2011 #12;What is a `proxy'? "Proxy, as used here

  12. Ensemble climate predictions using climate models and observational constraints

    E-Print Network [OSTI]

    REVIEW Ensemble climate predictions using climate models and observational constraints BY PETER A. STOTT 1,* AND CHRIS E. FOREST 2 1 Hadley Centre for Climate Change (Reading Unit), Meteorology Building for constraining climate predictions based on observations of past climate change. The first uses large ensembles

  13. Climate history and paleoclimate -HS 2011 Future climate

    E-Print Network [OSTI]

    Gilli, Adrian

    Climate history and paleoclimate - HS 2011 Future climate Climate History & Paleoclimate - December 9, 2011 1 #12;Climate history and paleoclimate - HS 2011 IPCC 2007 4th Assessment report (AR4) More information can be found: http://www.ipcc.ch/ Remark: 5th assessment report is due in 2013/2014 2 #12;Climate

  14. Climate Change: Conflict, Security and Vulnerability Professor of Climate Change

    E-Print Network [OSTI]

    Hulme, Mike

    Climate Change: Conflict, Security and Vulnerability Mike Hulme Professor of Climate Change Science, Society and Sustainability Group School of Environmental Sciences Rethinking Climate Change, Conflict security" "increase risk of conflicts among and within nations" #12;· from `climatic change' to `climate-change

  15. Sandia National Laboratories: Accelerated Climate Modeling for...

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Accelerated Climate Modeling for Energy New Project Is the ACME of Computer Science to Address Climate Change On December 3, 2014, in Analysis, Climate, Global Climate & Energy,...

  16. Old-field Community, Climate and Atmospheric Manipulation

    SciTech Connect (OSTI)

    Aimee Classen

    2009-11-01T23:59:59.000Z

    We are in the process of finishing a number of laboratory, growth chamber and greenhouse projects, analyzing data, and writing papers. The projects reported addressed these subjects: How do climate and atmospheric changes alter aboveground plant biomass and community structure; Effects of multiple climate changes factors on plant community composition and diversity: what did we learn from a 5-year open-top chamber experiment using constructed old-field communities; Do atmospheric and climatic change factors interact to alter woody seedling emergence, establishment and productivity; Soil moisture surpasses elevated CO{sub 2} and temperature in importance as a control on soil carbon dynamics; How do climate and atmospheric changes alter belowground root and fungal biomass; How do climate and atmospheric changes alter soil microarthropod and microbial communities; How do climate and atmospheric changes alter belowground microbial function; Linking root litter diversity and microbial functioning at a micro scale under current and projected CO{sub 2} concentrations; Multifactor climate change effects on soil ecosystem functioning depend on concurrent changes in plant community composition; How do climate and atmospheric changes alter aboveground insect populations; How do climate and atmospheric changes alter festuca endophyte infection; How do climate and atmospheric changes soil carbon stabilization.

  17. Climatic effects of nuclear war

    SciTech Connect (OSTI)

    Covey, C.

    1985-10-01T23:59:59.000Z

    Global climatic consequences of a nuclear war have, until recently, been assumed to be insignificant compared with the obviously devastating direct effects from blast, heat, and short-term fallout. But a number of investigations carried out over the past few years indicate that climatic impact could actually be severe enough to threaten the global ecosystem significantly, including regions that may not have been directly involved in the war. This change in perception comes as researchers realize that the fires ignited by nuclear explosions would generate so much smoke that, even spread over a large portion of Earth's surface, densities could be high enough to block most of the sunlight normally reaching the ground. As a result, temperatures could decrease below freezing in a nuclear winter lasting weeks to months. Smoke from fires is what would make nuclear winter so severe. Of necessity, theoretical models are relied upon to estimate the climatic impact of nuclear war. The models incorporate many uncertain assumptions, particularly regarding the small-scale details of smoke production by fires.

  18. ORNL/CDIAC-34 Carbon Dioxide Information Analysis Center and

    E-Print Network [OSTI]

    Research U.S. Department of Energy Budget Activity Number KP 12 04 01 0 Prepared by the Carbon Dioxide. Burtis Carbon Dioxide Information Analysis Center Environmental Sciences Division Publication No. 4777's (DOE) Environmental Sciences Division, Office of Biological and Environmental Research (OBER

  19. ORNL/CDIAC-57 Proceedings of RIHMI-WDC,

    E-Print Network [OSTI]

    and Environmental Research U.S. Department of Energy Budget Activity Number KP 05 00 00 0 Prepared by the Carbon Compiled by Marvel D. Burtis Carbon Dioxide Information Analysis Center Environmental Sciences Division Oak Prepared for the Global Change Research Program Environmental Sciences Division Office of Health

  20. ORNL/CDIAC-64 Proceedings of RIHMI-WDC,

    E-Print Network [OSTI]

    Research U.S. Department of Energy Budget Activity Number KP 05 00 00 0 Prepared by the Carbon Dioxide Compiled by Marvel D. Burtis Carbon Dioxide Information Analysis Center Environmental Sciences Division Oak for the #12;Global Change Research Program Environmental Sciences Division Office of Health and Environmental

  1. Carbon Dioxide Information Analysis Center (CDIAC)-Fossil Fuel...

    Open Energy Info (EERE)

    Kingdom, Uzbekistan, Iran, Kuwait, Qatar, Saudi Arabia, United Arab Emirates, Algeria, Egypt, South Africa, Australia, Bangladesh, China, India, Indonesia, Japan, Malaysia, New...

  2. Temperature, Temperature, Earth, geotherm for

    E-Print Network [OSTI]

    Treiman, Allan H.

    Temperature, Temperature, Earth, geotherm for total global heat flow Venus, geotherm for total global heat flow, 500 Ma #12;Temperature, Temperature, #12;Earth's modern regional continental geotherms Venusian Geotherms, 500 Ma Temperature, Temperature, After Blatt, Tracy, and Owens Petrology #12;Ca2Mg5Si8

  3. The Climate Impacts LINK Project

    E-Print Network [OSTI]

    Feigon, Brooke

    The Climate Impacts LINK Project The Climatic Research Unit, University of East Anglia Funded by the UK Department of the Environment, Transport and the Regions, Contract Ref EPG 1/1/68 The Climate Impacts LINK Project: Applying Results from the Hadley Centre's Climate Change Experiments for Climate

  4. Abrupt Climate Change Inevitable Surprises

    E-Print Network [OSTI]

    Abrupt Climate Change Inevitable Surprises Committee on Abrupt Climate Change Ocean Studies Board of Congress Cataloging-in-Publication Data Abrupt climate change : inevitable surprises / Committee on Abrupt Climate Change, Ocean Studies Board, Polar Research Board, Board on Atmospheric Sciences and Climate

  5. Climate Change Proposed Scoping Plan

    E-Print Network [OSTI]

    Climate Change Proposed Scoping Plan a amework for change Prepared by the California Air ResourcesBackgroundBackgroundBackground ............................................................................................................................................................................................................................................................................................................................................................................................................ 4444 1. Climate Change Policy in California1. Climate Change Policy in California1. Climate Change Policy in California1. Climate Change Policy in California

  6. Conservation and Global Climate Change

    E-Print Network [OSTI]

    Landweber, Laura

    V.6 Conservation and Global Climate Change Diane M. Debinski and Molly S. Cross OUTLINE 1. Introduction 2. How climate is changing 3. Environmental responses to climate change 4. Consequences of climate the coming decades will be preserving biodiversity in the face of climate change. It has become increasingly

  7. Tree Death Study's Climate Change Connections

    ScienceCinema (OSTI)

    McDowell, Nate

    2014-06-25T23:59:59.000Z

    What are the exact physiological mechanisms that lead to tree death during prolonged drought and rising temperatures? These are the questions that scientists are trying to answer at a Los Alamos National Laboratory research project called SUMO. SUMO stands for SUrvival/MOrtality study; it's a plot of land on the Lab's southern border that features 18 climate controlled tree study chambers and a large drought structure that limits rain and snowfall. Scientists are taking a wide variety of measurements over a long period of time to determine what happens during drought and warming, and what the connections and feedback loops might be between tree death and climate change.

  8. Tree Death Study's Climate Change Connections

    SciTech Connect (OSTI)

    McDowell, Nate

    2012-09-10T23:59:59.000Z

    What are the exact physiological mechanisms that lead to tree death during prolonged drought and rising temperatures? These are the questions that scientists are trying to answer at a Los Alamos National Laboratory research project called SUMO. SUMO stands for SUrvival/MOrtality study; it's a plot of land on the Lab's southern border that features 18 climate controlled tree study chambers and a large drought structure that limits rain and snowfall. Scientists are taking a wide variety of measurements over a long period of time to determine what happens during drought and warming, and what the connections and feedback loops might be between tree death and climate change.

  9. Global climatic catastrophes

    SciTech Connect (OSTI)

    Budyko, M.I.; Golitsyn, G.S.; Izrael, A

    1988-01-01T23:59:59.000Z

    This work inquires into global climatic catastrophes of the past, presenting data not easily available outside of the Socialist Countries, and applies these results to the study of future climatic developments, especially as they threaten in case of Nuclear Warfare - Nuclear Winter. The authors discuss probable after effects from the Soviet point of view on the basis of research, stressing the need to avoid all conflict which might lead to the next and final Global Climatic Catastrophy.

  10. Climate Action Plan (Virginia)

    Broader source: Energy.gov [DOE]

    Governor Timothy M. Kaine established the Governor's Commission on Climate Change in December 2007. The commission prepared a plan for Virginia that identified ways to reduce greenhouse gas...

  11. Sandia National Laboratories: Climate

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    from improved climate models to performance models for underground waste storage to 3D printing and digital rock physics. Marianne Walck (Director ... NASA Award for Marginal...

  12. Climate Change, Drought & Environment

    Broader source: Energy.gov [DOE]

    Afternoon Plenary Session: Current Trends in the Advanced Bioindustry Climate Change, Drought, and Environment—Michael Champ, Executive Director, The Sustainable Water Challenge

  13. Climate Vision: Presidential Statements

    Office of Scientific and Technical Information (OSTI)

    Remarks by the President at Major Economies Meeting on Energy Security and Climate Change September 28, 2007 THE PRESIDENT: Good morning. Thank you. Welcome to the State...

  14. Protecting climate with forests.

    E-Print Network [OSTI]

    2008-01-01T23:59:59.000Z

    much more than carbon sequestration does, and often in abiophysics, carbon sequestration, climate change, climatethe accompanying carbon sequestration does—and sometimes in

  15. Sandia National Laboratories: Climate

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Carbon Management On January 27, 2011, in A growing consensus exists among climate scientists, economists, and policy makers that the link between man-made emissions of greenhouse...

  16. Sandia National Laboratories: Climate

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Protected: White House Water Roundtable: Question 4 On September 20, 2011, in Climate, Water There is no excerpt because this is a protected post. Protected: White House Water...

  17. Welcome to Climate VISION

    Office of Scientific and Technical Information (OSTI)

    Program Mission Private Sector Initiatives Asia Pacific Partnership ClimateTechnology.gov Resources and Links 1605(b) Site Map Technology Pathways Contact Us News and Events How...

  18. ClimateChangeLIVE Webcast: Join the Climate Conversation

    Broader source: Energy.gov [DOE]

    Join ClimateChangeLIVE's webcast, bringing together students and climate experts for a discussion about climate change and what students and classes around the country are doing to be part of the climate solution. Students will be able to interact with climate scientists and experts online through Facebook and Twitter. A GreenWorks! grant will be offered to help schools with climate action projects.

  19. 1DANGEROUS CLIMATE CHANGE IN BRAZIL Dangerous Climate

    E-Print Network [OSTI]

    1DANGEROUS CLIMATE CHANGE IN BRAZIL Dangerous Climate A BrAzil-UK AnAlysis of ClimAte ChAnge And deforestAtion impACts in the AmAzon Change in Brazil #12;3DANGEROUS CLIMATE CHANGE IN BRAZIL April 2011Alysis of ClimAte ChAnge And deforestAtion impACts in the AmAzon Change in Brazil #12;4 DANGEROUS CLIMATE CHANGE

  20. Climatic effects of nuclear war

    SciTech Connect (OSTI)

    Turco, R.P.; Toon, O.B.; Ackerman, T.P.; Pollack, J.B.; Sagan, C.

    1984-08-01T23:59:59.000Z

    Recent findings by this group confirmed by workers in Europe, the US and the USSR, suggest that the long-term climatic effects of a major nuclear war are likely to be much severer and farther-reaching than had been supposed. In the aftermath of such a war vast areas of the earth could be subjected to prolonged darkness, abnormally low temperatures, violent windstorms, toxic smog and persistent radioactive fallout - in short, the combination of conditions that has come to be known as nuclear winter. In brief, the authors' initial results, published in Science in December, 1983, showed that the potential global atmospheric and climatic consequences of nuclear war...are serious. Significant hemispherical attenuation of the solar radiation flux and subfreezing land temperatures may be caused by fine dust raised in high-yield nuclear surface bursts and by smoke from city and forest fires ignited by airbursts of all yields. Subsequent studies, based on more powerful models of the general circulation of the earth's atmosphere, have tended to confirm both the validity of the authors' investgative approach and the main thrust of their findings. Most of this article is devoted to reviewing the current state of knowledge on this vital issue.

  1. Global air quality and climate

    E-Print Network [OSTI]

    2012-01-01T23:59:59.000Z

    Evaluation of Chemistry- Climate Models 5, 2010. 320 S. Wu,and R. Van Dorland, in Climate Change 2007: The PhysicalInter- governmental Panel on Climate Change, ed. D. Qin, M.

  2. Climate Change at Annual Timescales

    E-Print Network [OSTI]

    Stine, Alexander Robin

    2010-01-01T23:59:59.000Z

    1900–93, Journal of Climate, 10 (5), 1004–1020, 1997. Zhou,University of East Anglia’s Climate Research Unit (Jones etand those from WCRP “Climate of the Twentieth Century”

  3. MAPPING CLIMATE CHANGE EXPOSURES, VULNERABILITIES,

    E-Print Network [OSTI]

    MAPPING CLIMATE CHANGE EXPOSURES, VULNERABILITIES, AND ADAPTATION TO PUBLIC HEALTH RISKS's California Climate Change Center JULY 2012 CEC5002012041 Prepared for: California Energy Commission of California. #12; ii ABSTRACT This study reviewed first available frameworks for climate change adaptation

  4. Tropical CycloneInduced Upper-Ocean Mixing and Climate: Application to Equable Climates

    E-Print Network [OSTI]

    Emanuel, Kerry A.

    ), and above-freezing temperatures at polar latitudes were common through a significant fraction are principally responsible for transport- ing enthalpy poleward in the present climate, itself varies (CO2; Barron and Washington 1985), strong ocean heat transport (Barron 1983; Emanuel 2002; Korty 2005

  5. CLIMATE SCIENCE The Community Climate System Model results from a multi-agency collaboration

    E-Print Network [OSTI]

    Long, Nicholas

    . Could global warming be responsible for the July 2006 heat waves in Europe and the United States? Should- ter(NCDC),whicharchivesallweatherdataforthe nation, reports that global surface temperatures have, the DOEisdedicatedtoadvancingclimateresearchin order to elucidate the causes of climate change, includingtheroleofcarbonloadingfromfossilfuel use

  6. Climate Sciences: Atmospheric Thermodynamics

    E-Print Network [OSTI]

    Russell, Lynn

    1 Climate Sciences: Atmospheric Thermodynamics Instructor: Lynn Russell, NH343 http://aerosol.ucsd.edu/courses.html Text: Curry & Webster Atmospheric Thermodynamics Ch1 Composition Ch2 Laws Ch3 Transfers Ch12 Energy Climate Sciences: Atmospheric Thermodynamics Instructor: Lynn Russell, NH343 http

  7. As was hypothesized, annual ET water losses appears to be driven by seasonal variations in the total aboveground biomass of the treatment wetland. We found that only air temperature and PAR were significant climatic drivers of ET. However, unlike

    E-Print Network [OSTI]

    Hall, Sharon J.

    in the total aboveground biomass of the treatment wetland. We found that only air temperature and PAR were budget of an aridland" urban wastewater treatment wetland" Experimental Design and Field Sampling! · 10.T.A. 2003. Water and mass budgets of a vertical=-flow constructed wetland used for wastewater treatment

  8. Detection of CO sub 2 -induced climatic change

    SciTech Connect (OSTI)

    Wigley, T.M.L.; Jones, P.D.

    1990-07-15T23:59:59.000Z

    The aims of the US Department of Energy's CO{sub 2} Climate Research Program are to improve assessments of greenhouse-gas-induced climatic change and to define and reduce uncertainties through selected research. We propose to continue earlier work in five areas: updating, improvement and analysis of our global (land and marine) temperature data set; the development and use of multivariate techniques for the detection of greenhouse-gas-induced climatic change; the further development and use of simple transient-response climate models in order to elucidate the responses of the climate system to external and internal forcing; validation of General Circulation Models using a variety of test statistics, and the use of regression methods to produce sub-grid-scale information from GCM output. The present project addresses all of these questions. This document contains information of the progress in each area. 25 refs., 2 figs., 2 tabs.

  9. Dealing in Doubt: The Climate Denial Industry and Climate Science

    E-Print Network [OSTI]

    Fairchild, Mark D.

    Dealing in Doubt: The Climate Denial Industry and Climate Science A Brief History of Attacks action on climate change has become more likely. This time, though, there is a difference. In recent, despite its lack of evidence or scientific support. The last peak in the climate denial campaign

  10. Climate simulators and climate projections Jonathan Rougier1

    E-Print Network [OSTI]

    Dixon, Peter

    Climate simulators and climate projections Jonathan Rougier1 Department of Mathematics University;Abstract We provide a statistical interpretation of current practice in climate mod- elling. This includes: definitions for weather and climate; clarifying the relationship between simulator output and simulator

  11. The role of solar absorption in climate and climate change

    E-Print Network [OSTI]

    1 The role of solar absorption in climate and climate change William Collins UC Berkeley Research Boulder, Colorado, USA #12;2 Prior Research on Absorption and Climate Field Experiments: · Central · Climate with enhanced cloud absorption Synthesis of models and aerosol observations: · Development

  12. Global climatic change

    SciTech Connect (OSTI)

    Houghton, R.A.; Woodwell, G.M.

    1989-04-01T23:59:59.000Z

    This paper reviews the climatic effects of trace gases such as carbon dioxide and methane. It discusses the expected changes from the increases in trace gases and the extent to which the expected changes can be found in the climate record and in the retreat of glaciers. The use of ice cores in correlating atmospheric composition and climate is discussed. The response of terrestrial ecosystems as a biotic feedback is discussed. Possible responses are discussed, including reduction in fossil-fuel use, controls on deforestation, and reforestation. International aspects, such as the implications for developing nations, are addressed.

  13. Considerations for Energy Efficient Showers in Hot-Humid Climates

    E-Print Network [OSTI]

    Claridge, D. E.; Turner, W. D.

    1989-01-01T23:59:59.000Z

    CONSIDERATIONS FOR ENERGY EFFICIENT SHOWERS IN HOT-HUMID CLIMATES D. E. Claridge and W.D. Turner Energy Systems Laboratory Department of Mechanical Engineering Texas ALM University ABSTRACT Measurements have been conducted on four low... for typical operation in Texas. This has significant implications for everyone who purchases or uses showerheads; this is particularly true in hot climates where supply water temperatures are relatively high. TESTS CONDUCTED Showerheads Tested Two...

  14. Biological Impacts of Climate Change

    E-Print Network [OSTI]

    McCarty, John P.

    Biological Impacts of Climate Change John P McCarty, University of Nebraska at Omaha, Omaha, NE and reproduction depend on how well adapted individuals are to local climate patterns. Climate change can disrupt subsequent impacts on populations or species' distributions across geographic regions. Climate change may

  15. Climatic Change An Interdisciplinary, International

    E-Print Network [OSTI]

    Gvirtzman, Haim

    climate and cultural changes are observed in the Eastern Mediterranean and the Near East [e.g., Bookman et1 23 Climatic Change An Interdisciplinary, International Journal Devoted to the Description, Causes and Implications of Climatic Change ISSN 0165-0009 Volume 112 Combined 3-4 Climatic Change (2012) 112:769-789 DOI

  16. Wall Drying in Hot and Humid Climates

    E-Print Network [OSTI]

    Boone, K.; Weston, T.; Pascual, X.

    2004-01-01T23:59:59.000Z

    WALL DRYING IN HOT AND HUMID CLIMATES Kimdolyn Boone Theresa Weston, PhD Xuaco Pascual Product Development Engineer Building Scientist Field Services Engineer E.I. du Pont de Nemours and Company Richmond, VA ABSTRACT... time based on the varying weather conditions. Constant interior conditions of 70?F and 55% RH were chosen. This corresponds to typical interior temperatures and a high level of moisture production within the house. This was chosen as a worse...

  17. Regional analysis of ground and above-ground climate

    SciTech Connect (OSTI)

    Not Available

    1981-12-01T23:59:59.000Z

    The regional suitability of underground construction as a climate control technique is discussed with reference to (1) a bioclimatic analysis of long-term weather data for 29 locations in the United States to determine appropriate above ground climate control techniques, (2) a data base of synthesized ground temperatures for the coterminous United States, and (3) monthly dew point ground temperature comparisons for identifying the relative likelihood of condensation from one region to another. It is concluded that the suitability of earth tempering as a practice and of specific earth-sheltered design stereotypes varies geographically; while the subsurface almost always provides a thermal advantage on its own terms when compared to above ground climatic data, it can, nonetheless, compromise the effectiveness of other, regionally more important climate control techniques. Also contained in the report are reviews of above and below ground climate mapping schemes related to human comfort and architectural design, and detailed description of a theoretical model of ground temperature, heat flow, and heat storage in the ground. Strategies of passive climate control are presented in a discussion of the building bioclimatic analysis procedure which has been applied in a computer analysis of 30 years of weather data for each of 29 locations in the United States.

  18. Climate Change Adaptation Planning

    Office of Energy Efficiency and Renewable Energy (EERE)

    This course provides an introduction to planning for climate change impacts, with examples of tribes that have been going through the adaptation planning process. The course is intended for tribal...

  19. Cool Farming: Climate impacts

    E-Print Network [OSTI]

    Levi, Ran

    Cool Farming: Climate impacts of agriculture and mitigation potential greenpeace.org Campaigningfor meat categories as well as milk and selected plant products for comparison. 36 Figure 1: Total global

  20. Climate Action Plan (Michigan)

    Broader source: Energy.gov [DOE]

    On November 14, 2007, Governor Jennifer M. Granholm issued Executive Order No. 2007-42 establishing the Michigan Climate Action Council (MCAC). The Council is comprised of members representing...

  1. Refining climate models

    ScienceCinema (OSTI)

    Warren, Jeff; Iversen, Colleen; Brooks, Jonathan; Ricciuto, Daniel

    2014-06-26T23:59:59.000Z

    Using dogwood trees, Oak Ridge National Laboratory researchers are gaining a better understanding of the role photosynthesis and respiration play in the atmospheric carbon dioxide cycle. Their findings will aid computer modelers in improving the accuracy of climate simulations.

  2. Climate Action Plan (Minnesota)

    Broader source: Energy.gov [DOE]

    Recognizing the implications that global climate change may have on the economy, environment and quality of life in Minnesota, Governor Tim Pawlenty signed into law the 2007 Next Generation Energy...

  3. Refining climate models

    SciTech Connect (OSTI)

    Warren, Jeff; Iversen, Colleen; Brooks, Jonathan; Ricciuto, Daniel

    2012-10-31T23:59:59.000Z

    Using dogwood trees, Oak Ridge National Laboratory researchers are gaining a better understanding of the role photosynthesis and respiration play in the atmospheric carbon dioxide cycle. Their findings will aid computer modelers in improving the accuracy of climate simulations.

  4. Climate VISION: Events

    Office of Scientific and Technical Information (OSTI)

    Efficiency and CO2 Intensity Improvement (PDF 24 KB) October 24-26, 2005 12th Annual EPA Natural Gas STAR Workshop September 28-30, 2005 Climate RESOLVE GHG Management Workshop...

  5. Andreas Sterl, SEAMOCS, Malta, 17.03.2009 Hot temperatures and storm surges

    E-Print Network [OSTI]

    Haak, Hein

    Andreas Sterl, SEAMOCS, Malta, 17.03.2009 Hot temperatures and storm surges: Modelling the change #12;Andreas Sterl, SEAMOCS, Malta, 17.03.2009 Climate ­ what's that? Climate = statistics of weather" #12;Andreas Sterl, SEAMOCS, Malta, 17.03.2009 The climate system AR4, FAQ 1.2, Fig. 1 #12;Andreas

  6. Atmospheric Radiation Measurement Climate Research Facility (ACRF) Annual Report 2008

    SciTech Connect (OSTI)

    LR Roeder

    2008-12-01T23:59:59.000Z

    The Importance of Clouds and Radiation for Climate Change: The Earth’s surface temperature is determined by the balance between incoming solar radiation and thermal (or infrared) radiation emitted by the Earth back to space. Changes in atmospheric composition, including greenhouse gases, clouds, and aerosols, can alter this balance and produce significant climate change. Global climate models (GCMs) are the primary tool for quantifying future climate change; however, there remain significant uncertainties in the GCM treatment of clouds, aerosol, and their effects on the Earth’s energy balance. In 1989, the U.S. Department of Energy (DOE) Office of Science created the Atmospheric Radiation Measurement (ARM) Program to address scientific uncertainties related to global climate change, with a specific focus on the crucial role of clouds and their influence on the transfer of radiation in the atmosphere. To reduce these scientific uncertainties, the ARM Program uses a unique twopronged approach: • The ARM Climate Research Facility, a scientific user facility for obtaining long-term measurements of radiative fluxes, cloud and aerosol properties, and related atmospheric characteristics in diverse climate regimes; and • The ARM Science Program, focused on the analysis of ACRF and other data to address climate science issues associated with clouds, aerosols, and radiation, and to improve GCMs. This report provides an overview of each of these components and a sample of achievements for each in fiscal year (FY) 2008.

  7. Hydrology: The Influence of Climate Change and/or Land Cover/Use Change Steven R. Fassnacht, Colorado State University

    E-Print Network [OSTI]

    Hydrology: The Influence of Climate Change and/or Land Cover/Use Change Steven R. Fassnacht. Precipitation and temperature are the main drivers of hydrological systems, which influence water availability in those temperatures has decreased. Hydrologic changes are occurring due to a changing climate. For snow

  8. Sandia National Laboratories: Climate/Environment

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    ClimateEnvironment ClimateEnvironment On January 27, 2011, in ClimateEnvironment Sensing and Monitoring Modeling and Analysis Carbon Management Water & Environment Publications...

  9. Climate Change Science Institute | Clean Energy | ORNL

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Climate Change Science Institute SHARE Climate Change Science Institute To advance understanding of the Earth system, describe the consequences of climate change, and evaluate and...

  10. Geoengineering the Earth's Climate

    ScienceCinema (OSTI)

    Google Tech Talks

    2009-09-01T23:59:59.000Z

    Emergency preparedness is generally considered to be a good thing, yet there is no plan regarding what we might do should we be faced with a climate emergency. Such an emergency could take the form of a rapid shift in precipitation patterns, a collapse of the great ice sheets, the imminent triggering of strong climate system feedbacks, or perhaps the loss of valuable ecosystems. Over the past decade, we have used climate models to investigate the potential to reverse some of the effects of greenhouse gases in the atmosphere by deflecting some incoming sunlight back to space. This would probably be most cost-effectively achieved with the placement of small particles in or above the stratosphere. Our model simulations indicate that such geoengineering approaches could potentially bring our climate closer to the state is was in prior to the introduction of greenhouse gases. This talk will present much of what is known about such geoengineering approaches, and raise a range of issues likely to stimulate lively discussion. Speaker: Ken Caldeira Ken Caldeira is a scientist at the Carnegie Institution Department of Global Ecology and a Professor (by courtesy) at the Stanford University Department of Environmental and Earth System Sciences. Previously, he worked for 12 years in the Energy and Environment Directorate at the Lawrence Livermore National Laboratory (Department of Energy). His research interests include the numerical simulation of Earth's climate, carbon, and biogeochemistry; ocean acidification; climate emergency response systems; evaluating approaches to supplying environmentally-friendly energy services; ocean carbon sequestration; long-term evolution of climate and geochemical cycles; and marine biogeochemical cycles. Caldeira has a B.A. in Philosophy from Rutgers College and an M.S. and Ph.D. in Atmospheric Sciences from New York University.

  11. alternating temperature preculture: Topics by E-print Network

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    A; Moi, L 2013-01-01 3 Warm Humid Climate: Methodology to Study Air Temperature Distribution: Mobile Phones Base Stations as Viable Alternative for Fixed Points Texas A&M...

  12. Regional Climate Model Projections for the State of Washington

    SciTech Connect (OSTI)

    Salathe, E.; Leung, Lai-Yung R.; Qian, Yun; Zhang, Yongxin

    2010-05-05T23:59:59.000Z

    Global climate models do not have sufficient spatial resolution to represent the atmospheric and land surface processes that determine the unique regional heterogeneity of the climate of the State of Washington. If future large-scale weather patterns interact differently with the local terrain and coastlines than current weather patterns, local changes in temperature and precipitation could be quite different from the coarse-scale changes projected by global models. Regional climate models explicitly simulate the interactions between the large-scale weather patterns simulated by a global model and the local terrain. We have performed two 100-year climate simulations using the Weather and Research Forecasting (WRF) model developed at the National Center for Atmospheric Research (NCAR). One simulation is forced by the NCAR Community Climate System Model version 3 (CCSM3) and the second is forced by a simulation of the Max Plank Institute, Hamburg, global model (ECHAM5). The mesoscale simulations produce regional changes in snow cover, cloudiness, and circulation patterns associated with interactions between the large-scale climate change and the regional topography and land-water contrasts. These changes substantially alter the temperature and precipitation trends over the region relative to the global model result or statistical downscaling. To illustrate this effect, we analyze the changes from the current climate (1970-1999) to the mid 21st century (2030-2059). Changes in seasonal-mean temperature, precipitation, and snowpack are presented. Several climatological indices of extreme daily weather are also presented: precipitation intensity, fraction of precipitation occurring in extreme daily events, heat wave frequency, growing season length, and frequency of warm nights. Despite somewhat different changes in seasonal precipitation and temperature from the two regional simulations, consistent results for changes in snowpack and extreme precipitation are found in both simulations.

  13. NEW WORK AND STUDY OPPORTUNITIES IN CLIMATE CHANGE Climate System Analysis Group (CSAG)

    E-Print Network [OSTI]

    Cohen, Ronald C.

    . - Postdoc: Climate modeling - Postdoc: Climate change information communication and dissemination - Research Associate: Climate change information communication and dissemination - PhD: Climate change information communication and dissemination - MSc/PhD: Physical science of climate change What to expect: Successful

  14. Debating Climate Change

    SciTech Connect (OSTI)

    Malone, Elizabeth L.

    2009-11-01T23:59:59.000Z

    Debating Climate Change explores, both theoretically and empirically, how people argue about climate change and link to each other through various elements in their arguments. As science is a central issue in the debate, the arguments of scientists and the interpretations and responses of non-scientists are important aspects of the analysis. The book first assesses current thinking about the climate change debate and current participants in the debates surrounding the issue, as well as a brief history of various groups’ involvements. Chapters 2 and 3 distill and organize various ways of framing the climate change issue. Beginning in Chapter 4, a modified classical analysis of the elements carried in an argument is used to identify areas and degrees of disagreement and agreement. One hundred documents, drawn from a wide spectrum of sources, map the topic and debate space of the climate change issue. Five elements of each argument are distilled: the authority of the writer, the evidence presented, the formulation of the argument, the worldview presented, and the actions proposed. Then a social network analysis identifies elements of the arguments that point to potential agreements. Finally, the book suggests mechanisms by which participants in the debate can build more general agreements on elements of existing agreement.

  15. Forest phenology and a warmer climate - Growing season extension in relation to climatic provenance

    SciTech Connect (OSTI)

    Gunderson, Carla A [ORNL; Edwards, Nelson T [ORNL; Walker, Ashley V [ORNL; O'Hara, Keiran H [ORNL; Campion, Christina M [ORNL; Hanson, Paul J [ORNL

    2012-01-01T23:59:59.000Z

    Predicting forest responses to warming climates relies on assumptions about niche and temperature sensitivity that remain largely untested. Observational studies have related current and historical temperatures to phenological shifts, but experimental evidence is sparse, particularly for autumn responses. A five-year field experiment exposed four deciduous forest species from contrasting climates (Liquidambar styraciflua, Quercus rubra, Populus grandidentata, and Betula alleghaniensis) to air temperatures 2 and 4 C above ambient controls. Impacts of year-round warming on bud burst (BB), senescence and abscission were evaluated in relation to thermal provenance. Leaves emerged earlier in all species, by an average of 6-9 days at +2 and +4 C. Magnitude of advance varied with species and year, but was larger for the first 2 C increment than the second. The effect of warming increased with early BB, favoring Liquidambar, from the warmest climate, but even BB in northern species advanced, despite temperatures well beyond those of the realized niche. Treatment differences in BB were poorly explained by temperature sums, which increased with treatment. In autumn, chlorophyll was retained an average of 4 and 7 days longer in +2 and +4 C treatments, and abscission delayed by 8 and 13 days. Species differences in autumn responses were marginally significant. Growing seasons in the warmer atmospheres were 6 - 28 days longer, with the least impact in Quercus. Results are compared with a 16-year record of canopy onset and offset in a nearby upland deciduous forest, where BB showed similar responsiveness to spring temperatures (2 - 4 days C-1). Offset dates in the stand tracked August-September temperatures, except when late summer drought caused premature senescence. The common garden-like experimental approach provides evidence that warming alone extends the growing season, at both ends, even if stand-level impacts are complicated by other environmental factors.

  16. Climate simulations and projections with a super-parameterized climate model

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Stan, Cristiana; Xu, Li

    2014-10-01T23:59:59.000Z

    The mean climate and its variability are analyzed in a suite of numerical experiments with a fully coupled general circulation model in which subgrid-scale moist convection is explicitly represented through embedded 2D cloud-system resolving models. Control simulations forced by the present day, fixed atmospheric carbon dioxide concentration are conducted using two horizontal resolutions and validated against observations and reanalyses. The mean state simulated by the higher resolution configuration has smaller biases. Climate variability also shows some sensitivity to resolution but not as uniform as in the case of mean state. The interannual and seasonal variability are better represented in themore »simulation at lower resolution whereas the subseasonal variability is more accurate in the higher resolution simulation. The equilibrium climate sensitivity of the model is estimated from a simulation forced by an abrupt quadrupling of the atmospheric carbon dioxide concentration. The equilibrium climate sensitivity temperature of the model is 2.77 °C, and this value is slightly smaller than the mean value (3.37 °C) of contemporary models using conventional representation of cloud processes. The climate change simulation forced by the representative concentration pathway 8.5 scenario projects an increase in the frequency of severe droughts over most of the North America.« less

  17. Climate simulations and projections with a super-parameterized climate model

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Stan, Cristiana [George Mason Univ., Fairfax, VA (United States). Dept. of Atmospheric, Oceanic and Earth Sciences; Xu, Li [George Mason Univ., Fairfax, VA (United States). Center for Ocean-Land-Atmosphere Studies

    2014-10-01T23:59:59.000Z

    The mean climate and its variability are analyzed in a suite of numerical experiments with a fully coupled general circulation model in which subgrid-scale moist convection is explicitly represented through embedded 2D cloud-system resolving models. Control simulations forced by the present day, fixed atmospheric carbon dioxide concentration are conducted using two horizontal resolutions and validated against observations and reanalyses. The mean state simulated by the higher resolution configuration has smaller biases. Climate variability also shows some sensitivity to resolution but not as uniform as in the case of mean state. The interannual and seasonal variability are better represented in the simulation at lower resolution whereas the subseasonal variability is more accurate in the higher resolution simulation. The equilibrium climate sensitivity of the model is estimated from a simulation forced by an abrupt quadrupling of the atmospheric carbon dioxide concentration. The equilibrium climate sensitivity temperature of the model is 2.77 °C, and this value is slightly smaller than the mean value (3.37 °C) of contemporary models using conventional representation of cloud processes. The climate change simulation forced by the representative concentration pathway 8.5 scenario projects an increase in the frequency of severe droughts over most of the North America.

  18. Direct climate effect of black carbon in China and its impact on dust storms

    E-Print Network [OSTI]

    Liou, K. N.

    Click Here for Full Article Direct climate effect of black carbon in China and its impact on dust aerosols in China, particularly black carbon (BC), is the primary reason for precipitation and temperature, W. Chen, and H. Liao (2010), Direct climate effect of black carbon in China and its impact on dust

  19. A mechanism for sun-climate connection Sultan Hameed and Jae N. Lee

    E-Print Network [OSTI]

    Hameed, Sultan

    ]. Systematic changes in the distribution of ozone result in changes in the temperature and pressureA mechanism for sun-climate connection Sultan Hameed and Jae N. Lee Institute for Terrestrial in the sun's energy output during the solar cycle can cause changes in weather and climate have been a puzzle

  20. LOCAL UNDERSTANDING OF HYDRO-CLIMATE CHANGES IN MONGOLIA Submitted by

    E-Print Network [OSTI]

    MacDonald, Lee

    THESIS LOCAL UNDERSTANDING OF HYDRO-CLIMATE CHANGES IN MONGOLIA Submitted by Tumenjargal Sukh 2012 All Rights Reserved #12;ABSTRACT LOCAL UNDERSTANDING OF HYDRO-CLIMATE CHANGES IN MONGOLIA Air temperatures have increased more in semi-arid regions than in many other parts of the world. Mongolia has

  1. A Vast Machine Computer Models, Climate Data, and the Politics of Global Warming

    E-Print Network [OSTI]

    A Vast Machine Computer Models, Climate Data, and the Politics of Global Warming Paul N. Edwards models, climate data, and the politics of global warming / Paul N. Edwards. p. cm. Includes. Climatology--History. 3. Meteorology--History. 4. Climatology--Technological innovation. 5. Global temperature

  2. Climate Change, Mortality, and Adaptation: Evidence from Annual Fluctuations in Weather in the U.S.

    E-Print Network [OSTI]

    Deschenes, Olivier

    This paper produces the first large-scale estimates of the U.S. health related welfare costs due to climate change. Using the presumably random year-to-year variation in temperature and two state of the art climate models, ...

  3. UK Climate Change Risk Assessment and National

    E-Print Network [OSTI]

    Wirosoetisno, Djoko

    UK Climate Change Risk Assessment and National Adaptation Programme Meg Patel Defra #12 change #12;Weather & climate impacts - economic, societal, environmental Water consumption per capita;Legislative Framework Climate Change Act 2008 Adaptation Reporting Power 2011 Climate Change Risk Assessment

  4. COPENHAGEN CONSENSUS ON CLIMATE A Perspective Paper on Climate

    E-Print Network [OSTI]

    Colorado at Boulder, University of

    of Carbon Capture as a Response to Climate Change Roger Pielke, Jr. #12;COPENHAGEN CONSENSUS ON CLIMATE Engineering, Including an Analysis of Carbon Capture as a Response to Climate Change #12;AbstrAct PReface but not accurate. Second, it summarizes an analysis of the potential role for air capture technologies to play

  5. Climate Extremes, Uncertainty and Impacts Climate Change Challenge: The Fourth Assessment Report of the Intergovernmental Panel on Climate Change

    E-Print Network [OSTI]

    Climate Extremes, Uncertainty and Impacts Climate Change Challenge: The Fourth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC, AR4) has resulted in a wider acceptance of global climate change climate extremes and change impacts. Uncertainties in process studies, climate models, and associated

  6. Status of Climate Change

    E-Print Network [OSTI]

    North, G.

    2013-01-01T23:59:59.000Z

    Status of Climate Change 2013 CaTee Conference San Antonio 2013 ESL-KT-13-12-56 CATEE 2013: Clean Air Through Energy Efficiency Conference, San Antonio, Texas Dec. 16-18 Menu for Today • IPCC 2013: Assessment Report #5 • Facts about Climate Change... • Who will Win, Who will Lose • What Needs to be Done ESL-KT-13-12-56 CATEE 2013: Clean Air Through Energy Efficiency Conference, San Antonio, Texas Dec. 16-18 IPCC #5 • No great surprises - Sharper language • Uncertainties are still large • Essentially...

  7. Climate change cripples forests

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0ClimateClimate Change

  8. Climate change cripples forests

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0ClimateClimate

  9. Climate Change | Department of Energy

    Broader source: Energy.gov (indexed) [DOE]

    Climate Change Climate Change September 16, 2014 C3E Spotlights Women Leaders in Clean Energy Careers Women clean energy leaders convene in Boston for the Women in Clean Energy...

  10. Session Title Climate Smart Agriculture

    E-Print Network [OSTI]

    Barnes, Elizabeth A.

    Session Title Climate Smart Agriculture Session Date Khosla (moderator) Professor, Soil and Crop Sciences College of Agricultural Climate Smart Agriculture is a multi-disciplinary approach to practice agriculture

  11. Climate Change and National Security

    E-Print Network [OSTI]

    Alyson, Fleming; Summer, Kelly; Summer, Martin; Lauren, Franck; Jonathan, Mark

    2015-01-01T23:59:59.000Z

    of climate change, energy security and economic stability.DoD is improving U.S. energy security and national security.www.greenpacks.org • Energy Security & Climate Change:

  12. Climate Action Plan (New Orleans)

    Broader source: Energy.gov [DOE]

    New Orleans' Climate Action Plan will provide a road map to reach the City's greenhouse gas (GHG) reduction goal by 2030 while orchestrating its adaptation to climate change. The CAP will outline...

  13. Climate Action Plan (Ontario, Canada)

    Broader source: Energy.gov [DOE]

    Climate Ready, Ontario's Adaptation Strategy and Action Plan, outlines the problems, goals, and key strategies for the province's approach to climate change and the problems it poses. The Plan...

  14. Farming: A Climate Change Culprit

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Farming: A Climate Change Culprit Farming: A Climate Change Culprit Simulations run at NERSC show impact of land-use change on African monsoon precipitation June 7, 2014 | Tags:...

  15. Climate shocks: Natural and anthropogenic

    SciTech Connect (OSTI)

    Kondratyev, K.Ya.

    1988-01-01T23:59:59.000Z

    Much recent climate research has focused on the effects of CO{sub 2} and radiatively important trace species, volcanic eruptions, and nuclear exchanges on our future climate. These studies suggest that anthropogenic influence will alter our present climate. The reliability of the climate models are a subject of debate, yet valid information derived from climate models is critical for policy-makers and politicians to make decisions regarding energy use and development and defense strategies. K.Ya. Kondratyev, a leading Soviet climate scientist, addresses the role of the greenhouse effect, nuclear winter, and volcanic eruptions on our climate in a recently published book entitled Climate Shocks: Natural and Anthropogenic. The book provides a detailed survey of the literature on these fields, including the pertinent Soviet literature that is often not surveyed by Western scientists.

  16. Water vapor and the dynamics of climate changes

    E-Print Network [OSTI]

    Schneider, Tapio; Levine, Xavier

    2009-01-01T23:59:59.000Z

    Water vapor is not only Earth's dominant greenhouse gas. Through the release of latent heat when it condenses, it also plays an active role in dynamic processes that shape the global circulation of the atmosphere and thus climate. Here we present an overview of how latent heat release affects atmosphere dynamics in a broad range of climates, ranging from extremely cold to extremely warm. Contrary to widely held beliefs, atmospheric circulation statistics can change non-monotonically with global-mean surface temperature, in part because of dynamic effects of water vapor. For example, the strengths of the tropical Hadley circulation and of zonally asymmetric tropical circulations, as well as the kinetic energy of extratropical baroclinic eddies, can be lower than they presently are both in much warmer climates and in much colder climates. We discuss how latent heat release is implicated in such circulation changes, particularly through its effect on the atmospheric static stability, and we illustrate the circul...

  17. Detection of CO sub 2 -induced climatic change

    SciTech Connect (OSTI)

    Wigley, T.M.L.

    1990-07-15T23:59:59.000Z

    In spite of the strong circumstantial evidence that the greenhouse effect has contributed significantly to the observed global warming, we are still unable to state unequivocally that the effect has been detected. Either we must eliminate all other possibilities, or we must identify one or more multivariate characteristics of the observed changes in climate that are unique signature of the greenhouse effect. We propose to continue earlier work in five areas: Updating, improvement and analysis of our global (land and marine) temperature data set, The development and use of multivariate techniques for the detection of greenhouse-gas-induced climatic change, The further development and use of simple transient-response climate models in order to elucidate the responses of the climate system to external and internal forcing, Validation of General Circulation Models using a variety of test statistics, and The use of regression methods to produce sub-grid-scale information from GCM output. 63 refs., 2 figs., 1 tab.

  18. 1, 231253, 2005 Synoptic climate

    E-Print Network [OSTI]

    Boyer, Edmond

    CPD 1, 231­253, 2005 Synoptic climate change as driver of New Zealand glaciation H. Rother and J / Esc Print Version Interactive Discussion EGU Climate of the Past Discussions, 1, 231­253, 2005 www.climate-of-the-past.net/cpd/1/231/ SRef-ID: 1814-9359/cpd/2005-1-231 European Geosciences Union Climate of the Past Discussions

  19. Climate Action Plan (Manitoba, Canada)

    Broader source: Energy.gov [DOE]

    Manitoba's Climate Action Plan centers around energy efficiency, although it includes mandates and initiatives for renewable sources of energy.

  20. VISUAL ANALYTICS FOR CLIMATE ANDTEXT ANALYSIS

    E-Print Network [OSTI]

    Wang, Xiaorui "Ray"

    . Wednesday, April 11, 12 #12;CLIMATE DATA DELUGE Wednesday, April 11, 12 #12;CLIMATE DATA DELUGE Wednesday, April 11, 12 #12;CLIMATE DATA DELUGE Wednesday, April 11, 12 #12;CLIMATE DATA DELUGE Wednesday, April 11, 12 #12;CLIMATE DATA DELUGE Wednesday, April 11, 12 #12;CLIMATE DATA DELUGE Wednesday, April 11, 12

  1. Oregon Climate Assessment Report December 2010

    E-Print Network [OSTI]

    Pierce, Stephen

    - Climate change and agriculture in Oregon"" " " " " 151 Chapter 5 - The potential effects of climate changeOregon Climate Assessment Report December 2010 Oregon Climate Change Research Institute #12;Oregon Climate Assessment Report December 2010 Oregon Climate Change Research Institute Recommended citation

  2. An Assessment of the Impact of Climate Change on Hydroelectric Power 

    E-Print Network [OSTI]

    Harrison, Gareth P

    Global climate change is one of the greatest challenges of the twenty-first century. Rising temperatures and alteration of weather patterns are anticipated to result from increased atmospheric concentrations of greenhouse ...

  3. The Economic Impacts of Climate Change: Evidence from Agricultural Profits and Random Fluctuations of Weather

    E-Print Network [OSTI]

    Deschenes, Olivier.

    This paper measures the economic impact of climate change on agricultural land in the United States by estimating the effect of the presumably random year-to-year variation in temperature and precipitation on agricultural ...

  4. Geographic variation in vulnerability to climate warming in a tropical Caribbean lizard

    E-Print Network [OSTI]

    Leal, Manuel S.

    Geographic variation in vulnerability to climate warming in a tropical Caribbean lizard Alex R temperatures (Tb) of the tropical Caribbean lizard Anolis cristatellus at nine sites representing two habitat

  5. An examination of urban heat island characteristics in a global climate model

    E-Print Network [OSTI]

    Oleson, Keith W.; Bonan, Gordon B.; Feddema, Johannes J.; Jackson, Trisha L.

    2010-07-27T23:59:59.000Z

    A parameterization for urban surfaces has been incorporated into the Community Land Model as part of the Community Climate System Model. The parameterization allows global simulation of the urban environment, in particular the temperature of cities...

  6. Climate change impacts on freshwater recreational fishing in the United States

    E-Print Network [OSTI]

    Jones, Russell

    We estimated the biological and economic impacts of climate change on freshwater fisheries in the United States (U.S.). Changes in stream temperatures, flows, and the spatial extent of suitable thermal habitats for fish ...

  7. The role of US agricultural and forest activities in global climate change mitigation

    E-Print Network [OSTI]

    Zhu, En

    2009-05-15T23:59:59.000Z

    In 2005 the highest global surface temperature ever was recorded. A virtual consensus exists today among scientists that global warming is underway and that human greenhouse gas (GHG) emissions are a significant cause. Possible mitigation of climate...

  8. The economic impacts of climate change : evidence from agricultural profits and random fluctuations in weather

    E-Print Network [OSTI]

    Deschênes, Olivier

    2006-01-01T23:59:59.000Z

    This paper measures the economic impact of climate change on US agricultural land by estimating the effect of the presumably random year-to-year variation in temperature and precipitation on agricultural profits. Using ...

  9. EXAMINING VEGETATION AND CLIMATE INTERACTIONS: A COMPARATIVE STUDY OF DIFFERENT VEGETATION TYPES AND

    E-Print Network [OSTI]

    Wisconsin at Madison, University of

    . The mechanisms responsible for influencing the climate away from the surface, into the atmosphere, and to remote reduction in latent cooling. In contrast, boreal deforestation causes a large surface temperature cooling

  10. Climatic Change (2011) 106:315326 DOI 10.1007/s10584-010-9903-9

    E-Print Network [OSTI]

    2011-01-01T23:59:59.000Z

    an increase in surface temperature, decreasing the absorption of solar radiation, thereby diminishing and its probable uncertainty range as given by the Intergovernmental Panel on Climate Change (IPCC 2007

  11. SIMULATING THE IMPACTS OF CLIMATE CHANGE, PRICES AND POPULATION ON CALIFORNIA'S

    E-Print Network [OSTI]

    Auffhammer, Maximilian

    temperature bins on households' electricity consumption. The estimation uses a comprehensive household level of higher electricity prices and different scenarios of population growth. Finally, simulations wereSIMULATING THE IMPACTS OF CLIMATE CHANGE, PRICES AND POPULATION ON CALIFORNIA'S RESIDENTIAL

  12. BC Agriculture Climate Change Adaptation

    E-Print Network [OSTI]

    Pedersen, Tom

    BC Agriculture Climate Change Adaptation Risk + Opportunity Assessment Provincial Report executive summary #12;published March 2012 by the British Columbia Agriculture & Food Climate Action Initiative www.BCAgClimateAction.ca project funding provided by Agriculture and Agri-food Canada BC Ministry of Agriculture BC Ministry

  13. BC Agriculture Climate Change Adaptation

    E-Print Network [OSTI]

    Pedersen, Tom

    BC Agriculture Climate Change Adaptation Risk + Opportunity Assessment Provincial Report #12;published March 2012 by the British Columbia Agriculture & Food Climate Action Initiative www.BCAgClimateAction.ca project funding provided by Agriculture and Agri-food Canada BC Ministry of Agriculture BC Ministry

  14. Climate Change Major information sources

    E-Print Network [OSTI]

    ://www.ipcc.ch/ Vital Climate Graphics, at http://www.grida.no/climate/vital/ Climate Change Impacts on US, at http://www.gcrio.org/NationalAssessment/ Greenhouse Warming Prediction #12;Energy Predictions 2 Sources: Energy Information Administration (EIA); International Energy Agency (IEA) 2% growth per year, or doubling in 35 years (shortcut: 70/%=doubling) Fossil

  15. Climate Change Action Plan Report

    E-Print Network [OSTI]

    Hansen, Andrew J.

    Climate Change Action Plan Report Intermountain Region 2013 National Park Service Resource Stewardship and Science Landscape Conservation and Climate Change Division #12;About this Report Each National Park Service is responding to the challenge of climate change; and (2) raise awareness among NPS

  16. 4, 28752899, 2007 Climate change

    E-Print Network [OSTI]

    Paris-Sud XI, Université de

    HESSD 4, 2875­2899, 2007 Climate change impact and model inaccuracy P. Droogers et al. Title Page are under open-access review for the journal Hydrology and Earth System Sciences Climate change impact­2899, 2007 Climate change impact and model inaccuracy P. Droogers et al. Title Page Abstract Introduction

  17. CLIMATE CHANGE IMPACTS, VULNERABILITIES, AND

    E-Print Network [OSTI]

    CLIMATE CHANGE IMPACTS, VULNERABILITIES, AND ADAPTATION IN THE SAN FRANCISCO BAY AREA Commission's California Climate Change Center JULY 2012 CEC5002012071 Prepared for: California Energy, as well as projections of future changes in climate based on modeling studies using various plausible

  18. Climate Change Proposed Scoping Plan

    E-Print Network [OSTI]

    Climate Change Proposed Scoping Plan a amework for change Prepared by the California Air Resources #12;CLIMATE CHANGE SCOPING PLAN State of California Air Resources Board Resolution 08-47 December 11 greenhouse gas (GHG) emissions that cause global warming; WHEREAS, the adverse impacts of climate change

  19. Soil Water and Temperature System (SWATS) Handbook

    SciTech Connect (OSTI)

    Bond, D

    2005-01-01T23:59:59.000Z

    The soil water and temperature system (SWATS) provides vertical profiles of soil temperature, soil-water potential, and soil moisture as a function of depth below the ground surface at hourly intervals. The temperature profiles are measured directly by in situ sensors at the Central Facility and many of the extended facilities of the SGP climate research site. The soil-water potential and soil moisture profiles are derived from measurements of soil temperature rise in response to small inputs of heat. Atmospheric scientists use the data in climate models to determine boundary conditions and to estimate the surface energy flux. The data are also useful to hydrologists, soil scientists, and agricultural scientists for determining the state of the soil.

  20. Vegetation and climates in the Presidio basin, Texas

    E-Print Network [OSTI]

    Harris, Bruce Roahen

    1969-01-01T23:59:59.000Z

    with air temperatures, bu+ CPUR" TA BP. were found to nave temperatures 18 -P8 E;armor than . he ai&. Gates (19o6) had car1i ". - speculated that Lranspir tional cool' & g might reduce Lhe leaf temperature, t?ereby keeping the temperature of leaves... the movement of pesticide residue throughout i, he basin (Applegate, 1967). BTVDY AREA Presi dio County is located in West, Texas in the climatic region termed Trans-Pecos (Carr, 1967). The county is thc fourth la& gest in t' he state with an area of )&877...

  1. Sequential high temperature reduction, low temperature hydrolysis...

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    high temperature reduction, low temperature hydrolysis for the regeneration of sulfated NOx trap catalysts. Sequential high temperature reduction, low temperature hydrolysis for...

  2. CLIMATE POLICY The Planet's

    E-Print Network [OSTI]

    Falge, Eva

    CLIMATE POLICY The Planet's Laundromat The Planet's Laundromat ANTHROPOLOGY Rukina's Remarkable Planck Society's Science Express last fall as it began its trip through India. India's Prime Minister Man). As a mem- ber of the German delegation, the visit afford- ed me the opportunity to learn more about India

  3. ENERGY, CLIMATE AND SUSTAINABLE

    E-Print Network [OSTI]

    ENERGY, CLIMATE AND SUSTAINABLE DEVELOPMENT NAMAs and the Carbon Market Nationally Appropriate Mitigation Actions of developing countries PersPectives series 2009 #12;NAMAs and the Carbon MarketPPrOPriate MitigatiON actiONs: china's experience and Perspective . . . . . . . . . . . 11 Fei

  4. Energy, Climate & Infrastructure Security

    E-Print Network [OSTI]

    Energy, Climate & Infrastructure Security EXCEPTIONAL SERVICE IN THE NATIONAL INTEREST Sandia Security Administration under contract DE-AC04-94AL85000. SAND 2012-1846P CustomTraining Sandia providesPRAsandhowtheycanbemanaged to increase levels of safety and security. Like othertrainings,Sandiaexpertsdesigncoursesto beasbroadorin

  5. COLORADO CLIMATE Basic Climatology

    E-Print Network [OSTI]

    or cold, wetness or dryness, calm or storm, clearness or cloudiness Climate - the statistical collection;The Earth's Energy Balance Incoming energy from the sun (solar radiation) heats the Earth Some by the Earth and re-emitted Incoming solar radiation is shorter wavelengths (higher energy) than what

  6. aerosols and climate : uncertainties

    E-Print Network [OSTI]

    contributes to creating a level playing field. (BC emissions tradeble like CO2 emissions?) OUTLINE #12;size. policy measures, is even more uncertain (emissions & their chemical fingerprint are uncertain (not just aerosol emissions, not just climate impacts) OUTLINE #12;- Standardization doesn't reduce

  7. Global Climate & Catastrophic Risk

    E-Print Network [OSTI]

    de Lijser, Peter

    Global Climate & Catastrophic Risk Forum 2012 A Joint Program with LA RIMS Education Day Rethinking Catastrophic Risk in Risk Management: Earthquake-Related Challenges Featuring: Keynote Speaker Dr. Frank Beuthin, Willis Group Holdings Plc. Yohei Miyamoto, Aon Risk Solutions Curtis deVera, Marsh

  8. The Great Season Climatic Oscillation and the Global Warming

    E-Print Network [OSTI]

    Boucenna, Ahmed

    2008-01-01T23:59:59.000Z

    The present earth warming up is often explained by the atmosphere gas greenhouse effect. This explanation is in contradiction with the thermodynamics second law. The warming up by greenhouse effect is quite improbable. It is cloud reflection that gives to the earth s ground its 15 degres C mean temperature. Since the reflection of the radiation by gases is negligible, the role of the atmosphere greenhouse gases in the earth warming up by earth radiation reflection loses its importance. We think that natural climatic oscillations contribute more to earth climatic disturbances. The oscillation that we hypothesize to exist has a long period (800 to 1000 years). The glacier melting and regeneration cycles lead to variations in the cold region ocean water density and thermal conductibility according to their salinity. These variations lead one to think about a macro climate oscillating between maximum hot and minimum cold temperatures. This oscillation is materialized by the passages of the planet through hot, mil...

  9. Climate impacts on agriculture: Implications for crop production

    SciTech Connect (OSTI)

    Hatfield, Jerry L.; Boote, Kenneth J.; Kimball, B. A.; Ziska, Lewis A.; Izaurralde, Roberto C.; Ort, Don; Thomson, Allison M.; Wolfe, David W.

    2011-04-19T23:59:59.000Z

    Changes in temperature, CO2, and precipitation under the scenarios of climate change for the next 30 years present a challenge to crop production. This review focuses on the impact of temperature, CO2, and ozone on agronomic crops and the implications for crop production. Understanding these implications for agricultural crops is critical for developing cropping systems resilient to stresses induced by climate change. There is variation among crops in their response to CO2, temperature, and precipitation changes and, with the regional differences in predicted climate, a situation is created in which the responses will be further complicated. For example, the temperature effects on soybean could potentially cause yield reductions of 2.4% in the South but an increase of 1.7% in the Midwest. The frequency of years when temperatures exceed thresholds for damage during critical growth stages is likely to increase for some crops and regions. The increase in CO2 contributes significantly to enhanced plant growth and improved water use efficiency; however, there may be a downscaling of these positive impacts due to higher temperatures plants will experience during their growth cycle. A challenge is to understand the interactions of the changing climatic parameters because of the interactions among temperature, CO2, and precipitation on plant growth and development and also on the biotic stresses of weeds, insects, and diseases. Agronomists will have to consider the variations in temperature and precipitation as part of the production system if they are to ensure the food security required by an ever increasing population.

  10. Climate Change Impacts on Streamflow, Water Quality, and Best Management

    E-Print Network [OSTI]

    Nebraska-Lincoln, University of

    -efficient technologies A1B: a world with rapid economic growth based upon a balance of various energy sources Development locations Study Objectives: #12;Location of the Columbus, NE and Sioux City, IA climate stations Hydrologic Balance #12;Plant Growth Soil Temperature Pesticide Dynamics Nutrient Cycling Sedimentation Crop

  11. Arctic ozone loss and climate sensitivity: Updated threedimensional model study

    E-Print Network [OSTI]

    Feng, Wuhu

    Arctic ozone loss and climate sensitivity: Updated three­dimensional model study Chipperfield winter­spring chemical ozone loss from 1991 2003, its observed correlation with low temperatures. CTM throughout studied. The model reproduces large column winters also captures shape of ozone loss profile

  12. PHOTOSYNTHESIS AND GLOBAL CHANGE CAN CLIMATE DRIVEN CHANGES IN

    E-Print Network [OSTI]

    Barron-Gafford, Greg

    PHOTOSYNTHESIS AND GLOBAL CHANGE CAN CLIMATE DRIVEN CHANGES IN PHOTOSYNTHESIS BE USED TO PREDICT in photosynthesis, and thus substrate supply, influence the rate of ecosystem respiration (Re). Further- more in photosynthesis might result in concomitant changes in both the rate, and temperature-sensitivity, of Re. Re

  13. Mean Radiant Cooling in a Hot-Humid Climate

    E-Print Network [OSTI]

    Garrison, M.

    1996-01-01T23:59:59.000Z

    Shaded interior mass walls in a hot-humid climate can be thermally grounded to an earth heat sink under an insulated structure. The mean radiant temperature (MRT) of the shaded and thermally grounded interior mass walls will be cooler in summer than...

  14. Land degradation and climate change: a sin of omission?

    E-Print Network [OSTI]

    not solely responsible for the lack of awareness of the impacts of poor management practices, but we do play temperatures and the consequent increase in evaporative demand. During large rainfall events, land degradation a contributing role. At best, our increasing focus on climate change has an opportunity cost: there is less time

  15. Climate Dynamics manuscript No. (will be inserted by the editor)

    E-Print Network [OSTI]

    Codron, Francis

    -atmosphere coupling through surface heat fluxes, and is very easy to interpret. Exemples of studies in realistic)). As the temperature of a slab ocean is forced only by local surface heat fluxes, it will be very different fromClimate Dynamics manuscript No. (will be inserted by the editor) Ekman Heat Transport for Slab

  16. Simulations of Present and Future Climates in the Western United States with Four Nested Regional Climate Models

    SciTech Connect (OSTI)

    Duffy, Phil; Arritt, R.; Coquard, J.; Gutowski, William; Han, J.; Iorio, J.; Kim, Jongil; Leung, Lai R.; Roads, J.; Zeledon, E.

    2006-03-15T23:59:59.000Z

    We analyze simulations of present and future climates in the western U.S. performed with four regional climate models (RCMs) nested within two global ocean-atmosphere climate models. Our primary goal is to assess the range of regional climate responses to increased greenhouse gases in available RCM simulations. The four RCMs used different geographical domains, different increased greenhouse gas scenarios for future-climate simulations, and (in some cases) different lateral boundary conditions. For simulations of the present climate, we compare RCM results to observations and to results of the GCM that provided lateral boundary conditions to the RCM. For future-climate (increased greenhouse gas) simulations, we compare RCM results to each other and to results of the driving GCMs. When results are spatially averaged over the western U.S., we find that the results of each RCM closely follow those of the driving GCM in the same region, in both present and future climates. This is true even though the study area is in some cases a small fraction of the RCM domain. Precipitation responses predicted by the RCMs are in many regions not statistically significant compared to interannual variability. Where the predicted precipitation responses are statistically significant, they are positive. The models agree that near-surface temperatures will increase, but do not agree on the spatial pattern of this increase. The four RCMs produce very different estimates of water content of snow in the present climate, and of the change in this water content in response to increased greenhouse gases.

  17. Climate Change Mitigation: Climate, Health, and Equity Implications of the Visible and the Hidden

    E-Print Network [OSTI]

    Shonkoff, Seth Berrin

    2012-01-01T23:59:59.000Z

    2008). "Accountability of networked climate governance: Therise of transnational climate partnerships." GlobalBoard. CARB (2008d). Climate change proposed scoping plan: a

  18. Climate Change in the South American Monsoon System: Present Climate and CMIP5 Projections

    E-Print Network [OSTI]

    Jones, Charles; Carvalho, Leila M. V

    2013-01-01T23:59:59.000Z

    Lau, 1998: Does a monsoon climate exist over South America?J. Climate, 11, 1020–1040.America monsoon system. Climate Dyn. , 36, 1865–1880, doi:

  19. Climate Change Mitigation: Climate, Health, and Equity Implications of the Visible and the Hidden

    E-Print Network [OSTI]

    Shonkoff, Seth Berrin

    2012-01-01T23:59:59.000Z

    Board. CARB (2008d). Climate change proposed scoping plan: aJ. (2009). "Cities, Climate Change and Urban Heat Islandet al. (2006). Climate change in California: health,

  20. Bringing climate change down to earth : science and participation in Canadian and Australian climate change campaigns

    E-Print Network [OSTI]

    Padolsky, Miriam Elana

    2006-01-01T23:59:59.000Z

    about Global Climate Change. Public Understanding of ScienceFoundation. 2005a. Climate Change: A Matter of SurvivalFoundation. 2005b. Climate Change > Actions 2005 [cited 10

  1. Climate Change Mitigation: Climate, Health, and Equity Implications of the Visible and the Hidden

    E-Print Network [OSTI]

    Shonkoff, Seth Berrin

    2012-01-01T23:59:59.000Z

    impacts of climate change on California agriculture. Climateby climate change in California, such as agriculture areas agriculture. Without proactive climate change mitigation

  2. Climate Survey Original TemplateClimate Survey Original TemplateClimate Survey Original TemplateClimate Survey Original Template The Chair of the Department of DEPT NAME, NAME, is dedicated to improving workplace climate in your office. As part

    E-Print Network [OSTI]

    Sheridan, Jennifer

    Climate Survey Original TemplateClimate Survey Original TemplateClimate Survey Original TemplateClimate Survey Original Template The Chair of the Department of DEPT NAME, NAME, is dedicated to improving Survey Original TemplateClimate Survey Original TemplateClimate Survey Original TemplateClimate Survey

  3. Modeling the Summertime Climate of Southwest Asia: The Role of Land Surface Processes in Shaping the Climate of Semiarid Regions

    E-Print Network [OSTI]

    Marcella, Marc P.

    Presented is a study on the role of land surface processes in determining the summertime climate over the semiarid region of southwest Asia. In this region, a warm surface air temperature bias of 3.5°C is simulated in the ...

  4. Climate change and health: Indoor heat exposure in vulnerable populations

    SciTech Connect (OSTI)

    White-Newsome, Jalonne L., E-mail: jalonne@umich.edu [University of Michigan School of Public Health, Environmental Health Sciences Department, 109 S. Observatory, SPH II, Rm. M6314, Ann Arbor, MI 48109 (United States); Sanchez, Brisa N., E-mail: brisa@umich.edu [University of Michigan School of Public Health, Biostatistics Department, M4164 SPH II, 1415 Washington Heights, Ann Arbor, MI 48109-2029 (United States); Jolliet, Olivier, E-mail: ojolliet@umich.edu [University of Michigan School of Public Health, Environmental Health Sciences Department, 6622 SPH tower, 1415 Washington Heights, Ann Arbor, MI 48109-2029 (United States)] [University of Michigan School of Public Health, Environmental Health Sciences Department, 6622 SPH tower, 1415 Washington Heights, Ann Arbor, MI 48109-2029 (United States); Zhang, Zhenzhen, E-mail: zhzh@umich.edu [University of Michigan School of Public Health, Biostatistics Department, M4164 SPH II, 1415 Washington Heights, Ann Arbor, MI 48109-2029 (United States)] [University of Michigan School of Public Health, Biostatistics Department, M4164 SPH II, 1415 Washington Heights, Ann Arbor, MI 48109-2029 (United States); Parker, Edith A., E-mail: Edith-Parker@uiowa.edu [University of Michigan School of Public Health, Health Behavior and Health Education Department, 1415 Washington Heights, Ann Arbor, MI 48109-2029 (United States); Timothy Dvonch, J., E-mail: dvonch@umich.edu [University of Michigan School of Public Health, Environmental Health Sciences Department, 1415 Washington Heights, 6642 SPH Tower, Ann Arbor, MI 48109 (United States); O'Neill, Marie S., E-mail: marieo@umich.edu [University of Michigan School of Public Health, Environmental Health Sciences Department, 6631 SPH Tower, 1415 Washington Heights, Ann Arbor, MI 48109 (United States)

    2012-01-15T23:59:59.000Z

    Introduction: Climate change is increasing the frequency of heat waves and hot weather in many urban environments. Older people are more vulnerable to heat exposure but spend most of their time indoors. Few published studies have addressed indoor heat exposure in residences occupied by an elderly population. The purpose of this study is to explore the relationship between outdoor and indoor temperatures in homes occupied by the elderly and determine other predictors of indoor temperature. Materials and methods: We collected hourly indoor temperature measurements of 30 different homes; outdoor temperature, dewpoint temperature, and solar radiation data during summer 2009 in Detroit, MI. We used mixed linear regression to model indoor temperatures' responsiveness to weather, housing and environmental characteristics, and evaluated our ability to predict indoor heat exposures based on outdoor conditions. Results: Average maximum indoor temperature for all locations was 34.85 Degree-Sign C, 13.8 Degree-Sign C higher than average maximum outdoor temperature. Indoor temperatures of single family homes constructed of vinyl paneling or wood siding were more sensitive than brick homes to outdoor temperature changes and internal heat gains. Outdoor temperature, solar radiation, and dewpoint temperature predicted 38% of the variability of indoor temperatures. Conclusions: Indoor exposures to heat in Detroit exceed the comfort range among elderly occupants, and can be predicted using outdoor temperatures, characteristics of the housing stock and surroundings to improve heat exposure assessment for epidemiological investigations. Weatherizing homes and modifying home surroundings could mitigate indoor heat exposure among the elderly.

  5. Climate Change Impacts for the Conterminous USA: An Integrated Assessment Part 1. Scenarios and Context

    SciTech Connect (OSTI)

    Smith, Steven J.; Thomson, Allison M.; Rosenberg, Norman J.; Izaurralde, R Cesar C.; Brown, Robert A.; Wigley, T. M.

    2005-04-01T23:59:59.000Z

    As CO2 and other greenhouse gasses accumulate in the atmosphere and contribute to rising global temperatures, it is important to examine how a changing climate may affect natural and managed ecosystems. In this series of papers, we study the impacts of climate change on agriculture, water resources and natural ecosystems in the conterminous United States using a suite of climate change projections from General Circulation Models (GCMs) and three biophysical models. In this paper we present the climate change scenarios used to drive the impact analyses. The assumed levels of global-mean climate changes are discussed and placed in the context of recent work on climate-change scenarios for the next 100 years. The spatial variation of these changes given by the GCM results used for the impact analyses are also discussed.

  6. Climate-Energy Nexus

    SciTech Connect (OSTI)

    Gary Sayler; Randall Gentry; Jie Zhuang

    2010-07-01T23:59:59.000Z

    The 140-page published proceedings of the workshop include individual articles and PowerPoint slides for all workshop presentations. The proceedings also contain pertinent background information on the China-US Joint Research Center, partnering organizations, and workshop goals and objectives. Overall, the workshop increased the understanding of the impacts of climate change on energy use and renewable energy production as well as the complex relationships among land use, energy production, and ecological restoration. The workshop served as an international platform for scientists and students of different research backgrounds to develop a unified perspective on energy and climate relationships. Such understanding will benefit future cooperation between China and the US in mitigating global climate change. The workshop’s agenda, which is highly interdisciplinary, explored many potential opportunities for international collaboration in ecosystem management, climate modeling, greenhouse gas emissions, and bioenergy sustainability. International research groups have been suggested in the areas of genomes and biotechnology of energy plants, sustainable management of soil and water resources, carbon sequestration, and microbial processes for ecological cycles. The project has attracted considerable attention from institutes beyond the China-US Joint Research Center partners, and several of them (such as Institute of Qing-Tibet Plateau Research, Institute of Soil and Water Conservation, Institute of Applied Ecology, CAS) have expressed interest in joining the partnership. In addition, the workshop played a significant role in facilitating establishment of private-public partnerships between government and private bioenergy companies (such as L.R. Shugarts and Associates, Inc.), including seed providers (Blade Energy Crops, Thousand Oaks, CA), pilot demonstration projects at coal-producing cities (e.g., Huaibei, Anhui province, China), and the development of methodology for assessment of the sustainable production of biofuels (such as life-cycle analysis, sustainability metrics, and land-use policy). Establishment of two US-China scientific research networks in the area of bioenergy and environmental science is a significant result of the workshop.

  7. Carbon dioxide and climate

    SciTech Connect (OSTI)

    Not Available

    1990-10-01T23:59:59.000Z

    Scientific and public interest in greenhouse gases, climate warming, and global change virtually exploded in 1988. The Department's focused research on atmospheric CO{sub 2} contributed sound and timely scientific information to the many questions produced by the groundswell of interest and concern. Research projects summarized in this document provided the data base that made timely responses possible, and the contributions from participating scientists are genuinely appreciated. In the past year, the core CO{sub 2} research has continued to improve the scientific knowledge needed to project future atmospheric CO{sub 2} concentrations, to estimate climate sensitivity, and to assess the responses of vegetation to rising concentrations of CO{sub 2} and to climate change. The Carbon Dioxide Research Program's goal is to develop sound scientific information for policy formulation and governmental action in response to changes of atmospheric CO{sub 2}. The Program Summary describes projects funded by the Carbon Dioxide Research Program during FY 1990 and gives a brief overview of objectives, organization, and accomplishments.

  8. Delays in Reducing Waterborne and Water-related Infectious Diseases in China under Climate Change

    SciTech Connect (OSTI)

    Hodges, Maggie; Belle, Jessica; Carlton, Elizabeth; Liang, Song; Li, Huazhong; Luo, Wei; Freeman, Matthew C.; Liu, Yang; Gao, Yang; Hess, Jeremy; Remais, Justin V.

    2014-12-01T23:59:59.000Z

    Despite China’s rapid progress improving water, sanitation and hygiene (WSH) infrastructure and access, in 2011, 471 million people lacked access to improved sanitation, and 401 million people lacked access to household piped water. Infectious diseases are sensitive to changes in climate, particularly temperature, and WSH conditions. To explore possible impacts of climate change on these diseases in China in 2020 and 2030, we coupled estimates of the temperature sensitivity of diarrheal disease and three vector-borne diseases, temperature projections from global climate models using four emissions pathways, WSH-infrastructure development scenarios and projected demographic changes. By 2030, the projected impacts would delay China’s historically rapid progress toward reducing the burden of WSH-attributable infectious disease by 8-85 months. This developmental delay provides a key summary measure of the impact of climate change in China, and in other societies undergoing rapid social, economic, and environmental change.

  9. Sensitivity of climate models: Comparison of simulated and observed patterns for past climates. Progress report, February 1, 1992--January 31, 1993

    SciTech Connect (OSTI)

    Prell, W.L.; Webb, T. III

    1992-08-01T23:59:59.000Z

    Predicting the potential climatic effects of increased concentrations of atmospheric carbon dioxide requires the continuing development of climate models. Confidence in the predictions will be much enhanced once the models are thoroughly tested in terms of their ability to simulate climates that differ significantly from today`s climate. As one index of the magnitude of past climate change, the global mean temperature increase during the past 18,000 years is similar to that predicted for carbon dioxide--doubling. Simulating the climatic changes of the past 18,000 years, as well as the warmer-than-present climate of 6000 years ago and the climate of the last interglacial, around 126,000 years ago, provides an excellent opportunity to test the models that are being used in global climate change research. During the past several years, we have used paleoclimatic data to test the accuracy of the National Center for Atmospheric Research, Community Climate Model, Version 0, after changing its boundary conditions to those appropriate for past climates. We have assembled regional and near-global paleoclimatic data sets of pollen, lake level, and marine plankton data and calibrated many of the data in terms of climatic variables. We have also developed methods that permit direct quantitative comparisons between the data and model results. Our research has shown that comparing the model results with the data is an evolutionary process, because the models, the data, and the methods for comparison are continually being improved. During 1992, we have completed new modeling experiments, further analyzed previous model experiments, compiled new paleodata, made new comparisons between data and model results, and participated in workshops on paleoclimatic modeling.

  10. ``Climate Modelling & Global Change'' scientific report ``Climate Modelling & Global Change'' Team

    E-Print Network [OSTI]

    ``Climate Modelling & Global Change'' scientific report ``Climate Modelling & Global Change'' Team) : : : : : : : : : : : : : : : : : 6 2.2 Anthropogenic climate change studies: scenario experiments (96) : : : : : : : : : 7 2 following its creation, the ``Climate Modelling & Global Change'' team had to make its proofs in order

  11. ``Climate Modelling & Global Change'' scientific report 1 ``Climate Modelling & Global Change'' Team

    E-Print Network [OSTI]

    ``Climate Modelling & Global Change'' scientific report 1 ``Climate Modelling & Global Change of the tropical climate : : : : : : : : : : : : : : : : : : : : : 6 2.2 Short­term variability studies : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : 8 2.3 Climate drift sensitivity studies

  12. Trends `91: A compendium of data on global change---highlights

    SciTech Connect (OSTI)

    Boden, T.A.; Sepanski, R.J.; Stoss, F.W. [eds.

    1992-03-01T23:59:59.000Z

    The Carbon Dioxide Information Analysis Center (CDIAC) at Oak Ridge National Laboratory (ORNL) has been prompted to produce the series Trends, a concise inventory of data in response to heightened concern about global environmental issues, in particular climate changes induced by the greenhouse effect. This report contains extracts from Trends `91 to illustrate the content, style, and presentation of data contained in the full 700-page report. This report includes a listing of the investigators contributing data for Trends `91. In addition, it contains the abstract, foreword, and acknowledgments, as well as the introduction and a sample data record from each of the reports`s five chapters. The chapters are ``Atmospheric CO{sub 2},`` ``Atmospheric CH{sub 4},`` ``Other Trace Gases,`` ``CO{sub 2} Emissions,`` and ``Temperature.`` Appendix A provides information about CDIAC and its activities related to global environmental issues. Appendix B lists the contents of the full report. An order form for obtaining a free copy of Trends `91 is found in Appendix C.

  13. Trends '91: A compendium of data on global change---highlights

    SciTech Connect (OSTI)

    Boden, T.A.; Sepanski, R.J.; Stoss, F.W. (eds.)

    1992-03-01T23:59:59.000Z

    The Carbon Dioxide Information Analysis Center (CDIAC) at Oak Ridge National Laboratory (ORNL) has been prompted to produce the series Trends, a concise inventory of data in response to heightened concern about global environmental issues, in particular climate changes induced by the greenhouse effect. This report contains extracts from Trends '91 to illustrate the content, style, and presentation of data contained in the full 700-page report. This report includes a listing of the investigators contributing data for Trends '91. In addition, it contains the abstract, foreword, and acknowledgments, as well as the introduction and a sample data record from each of the reports's five chapters. The chapters are Atmospheric CO[sub 2],'' Atmospheric CH[sub 4],'' Other Trace Gases,'' CO[sub 2] Emissions,'' and Temperature.'' Appendix A provides information about CDIAC and its activities related to global environmental issues. Appendix B lists the contents of the full report. An order form for obtaining a free copy of Trends '91 is found in Appendix C.

  14. Presented by Climate Extremes: The Science,

    E-Print Network [OSTI]

    of climate change and impacts · Feedback among climate, land use, and population distribution · Climate Severe storms projected to grow more intense and frequent with changing climate 1. Observed trends match climate patterns and changing likelihoods of severe events, may bridge the gap · The challenge in going

  15. 4, 173211, 2008 Climate and glacier

    E-Print Network [OSTI]

    Boyer, Edmond

    CPD 4, 173­211, 2008 Climate and glacier response to ENSO in subtropical Andes E. Dietze et al.0 License. Climate of the Past Discussions Climate of the Past Discussions is the access reviewed discussion forum of Climate of the Past Response of regional climate and glacier ice proxies to El Ni

  16. Climate Change Adaptation for Local Government

    E-Print Network [OSTI]

    Pedersen, Tom

    Climate Change Adaptation for Local Government A Resource Guide June 2011 Jenny Fraser, Adaptation to Climate Change Team, Simon Fraser University #12;Page 1 of 26 Climate Change Adaptation for Local: RESOURCES THAT SUPPORT CLIMATE CHANGE ASSESSMENT 3. Past and Future Climate Change and Its Impacts 4

  17. Climate Change and Tourism Dr David Viner

    E-Print Network [OSTI]

    Feigon, Brooke

    Climate Change and Tourism éCLAT Dr David Viner Climatic Research Unit University of East Anglia d.viner@uea.ac.uk Tourism has a strong international dimension and is sensitive to any changes of climate that alter to attract visitors are likely to be vulnerable to climate change and the implementation of climate change

  18. CLIMATE CHANGE: Past, Present and Future: Introduction

    E-Print Network [OSTI]

    Allan, Richard P.

    CLIMATE CHANGE: Past, Present and Future: Introduction Richard Allan, Department of Meteorology r.p.allan@reading.ac.uk #12;Text Books and References · Henson, B., Rough Guide to Climate Change http://www.amazon.co.uk/Climate-Change-Guides-Reference- Titles/dp/1858281059 · Intergovernmental Panel on Climate Change (IPCC), Climate Change 2007, www

  19. Sandia National Laboratories: Climate Security

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    limit economic development, impact interdependent infrastructure (such as energy and agriculture), and are a fundamental source of ... Climate Security On May 13, 2011, in...

  20. Climate Action Plan (South Carolina)

    Broader source: Energy.gov [DOE]

    Governor Sanford issued Executive Order 2007-04 on February 16, 2007, establishing the South Carolina Climate, Energy and Commerce Advisory Committee (CECAC).

  1. Climate VISION: How to Participate

    Office of Scientific and Technical Information (OSTI)

    companies on the Climate VISION website. Many of these resources - including case studies, training courses, and more - are available to any company. We encourage your...

  2. Climate change risk and response

    E-Print Network [OSTI]

    Kahrl, Fredrich; Roland-Holst, David

    2008-01-01T23:59:59.000Z

    Impacts on California’s Water Supply Source Medellin-AzuaraClimate Change on Yields and Water use of Major Californiawith Less: Agricultural Water Conservation and Efficiency in

  3. Climate Action Plan (New Mexico)

    Broader source: Energy.gov [DOE]

    Recognizing the profound implications that global warming and climate variation could have on the economy, environment and quality of life in the Southwest, New Mexico Governor Bill Richardson...

  4. Climate Change and National Security

    E-Print Network [OSTI]

    Alyson, Fleming; Summer, Kelly; Summer, Martin; Lauren, Franck; Jonathan, Mark

    2015-01-01T23:59:59.000Z

    seas, droughts and fresh water shortages. ? Risk Assessmentinse- curity, water and food shortages, and climate-drivenalso struggle with shortages in fresh water, food and other

  5. Massachusetts Takes On Climate Change

    E-Print Network [OSTI]

    Kimmell, Ken; Laurie, Burt

    2009-01-01T23:59:59.000Z

    consumers and business with their energy costs by removingintegrated energy and climate policies lead to real businessas for energy efficiency measures in homes, businesses and

  6. Climate Change, Adaptation, and Development

    E-Print Network [OSTI]

    Cole, Daniel H.

    2008-01-01T23:59:59.000Z

    climate change is coal gasification, which can make theworld leaders in coal gasification tech- nology, has beenexperimenting with "in situ" gasification, where the coal is

  7. Sandia National Laboratories: Climate change

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    research effort. Created to help resolve scientific uncertainties related to global climate change, ARM focuses on studying the role of clouds and aerosols in atmospheric and...

  8. Climate Change, Adaptation, and Development

    E-Print Network [OSTI]

    Cole, Daniel H.

    2008-01-01T23:59:59.000Z

    climate change is coal gasification, which can make thethe world leaders in coal gasification tech- nology, haswill not occur. If not coal gasification, then perhaps fuel

  9. Long-term climate variability and abrupt climate change Instructor: Dr. Igor Kamenkovich, associate professor

    E-Print Network [OSTI]

    Miami, University of

    Long-term climate variability and abrupt climate change Instructor: Dr. Igor Kamenkovich, associate students to learn about existing theories of abrupt climate changes and climate variability on time scales of long-term climate variability and abrupt climate change. This course compliments current MPO courses

  10. Gravity Recovery And Climate Experiment Hydrology, Earth Science and Climate

    E-Print Network [OSTI]

    Mosegaard, Klaus

    · GRACE and Geophysics ­ 2004 Sumatra Earthquake · GRACE and Climate Change ­ East Greenland Melting ­ Observe changes with unprecidented accuracy GRACE can not discriminate between sources/causes Water: Atmosphere (Transport of water, pressure) Climate (Glaciers, Ice mass melting -> Run off) Hydrology

  11. Sea Level Rise Adaptation: From Climate Chaos to Climate Resilience

    E-Print Network [OSTI]

    Rohs, Remo

    Sea Level Rise Adaptation: From Climate Chaos to Climate Resilience Human Dimensions and Ocean, 2013 #12;Main Discussion Points · How do we incorporate Sea-Level Rise into planning and regulatory actions? · What Does the new NRC Report on Sea- Level Rise mean to Decision-makers? · How does Sea-Level

  12. Climate Change Response

    Office of Environmental Management (EM)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742 33 1112011AT&T, Inc.'sEnergyTexas1. FeedstockCLEAN AIR ACT §CleantechClimate ChangeInterior

  13. Climate Data Operators (CDO)

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0Climate Change: Effects

  14. Climate change cripples forests

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0Climate

  15. Sandia Energy - Climate

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level:Energy: Grid Integration Redefining What's PossibleRadiation Protection245C Unlimited ReleaseWelcomeLong Lifetime of KeyCarbonSandiaClimate

  16. ARM Climate Research Facility

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWP TWP Related Links Facilities andPastWritten Records5 ARM Climate

  17. ARM Climate Research Facility

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWP TWP Related Links Facilities andPastWritten Records5 ARM Climate3 ARM

  18. ARM Climate Research Facility

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWP TWP Related Links Facilities andPastWritten Records5 ARM Climate3 ARM

  19. ARM Climate Research Facility

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWP TWP Related Links Facilities andPastWritten Records5 ARM Climate3

  20. ARM Climate Research Facility

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWP TWP Related Links Facilities andPastWritten Records5 ARM Climate38

  1. ARM Climate Research Facility

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWP TWP Related Links Facilities andPastWritten Records5 ARM Climate383

  2. Editors Kirsten Halsns & Amit Garg ENERGY, CLIMATE

    E-Print Network [OSTI]

    Editors Kirsten Halsnæs & Amit Garg ENERGY, CLIMATE Sustainable Development, Energy and Climate Development, Energy and Climate Exploring Synergies and Tradeoffs Methodological Issues and Case Studies from Brazil, China, India, South Africa, Bangladesh and Senegal Editors Kirsten Halsnæs & Amit Garg ENERGY

  3. POTENTIAL IMPACTS OF CLIMATE CHANGE ON

    E-Print Network [OSTI]

    Sheridan, Jennifer

    POTENTIAL IMPACTS OF CLIMATE CHANGE ON FLOODING IN WISCONSIN Ken Potter and Zach Schuster flood scenarios in Wisconsin · Potential impact of climate change on Wisconsin flooding · Ongoing #12;WISCONSIN INITIATIVE ON CLIMATE CHANGE IMPACTS · Partnership between the University of Wisconsin

  4. Climate Change and Place Roundtable Discussion

    E-Print Network [OSTI]

    2008-01-01T23:59:59.000Z

    of Urban Development and Climate Change,” 2007. The fullThink about what runaway climate change would mean where youWorld Changing Seattle, WA Climate change is global in scale

  5. CLIMATE VULNERABILITY AND ADAPTATION STUDY FOR

    E-Print Network [OSTI]

    CLIMATE VULNERABILITY AND ADAPTATION STUDY FOR CALIFORNIA Legal Analysis of Barriers's California Climate Change Center JULY 2012 CEC5002012019 Prepared for: California Energy Commission to that framework that would facilitate adaptation to climate change. Since such changes may be difficult

  6. Climate Workshops for Department Chairs Introduction

    E-Print Network [OSTI]

    Sheridan, Jennifer

    #12;Climate Workshops for Department Chairs Introduction Why focus on Department Chairs? Goals participating departments Evidence from Campus-wide Climate Surveys #12;Why focus on Department Chairs? Individuals experience climate in their immediate workplace ­ the department Chairs can significantly

  7. Climate policy and dependence on traded carbon

    E-Print Network [OSTI]

    Andrew, Robbie M; Davis, Steven J; Peters, Glen P

    2013-01-01T23:59:59.000Z

    Contact us My IOPscience Climate policy and dependence on10.1088/1748-9326/8/3/034011 Climate policy and dependenceCenter for International Climate and Environmental Research—

  8. CLIMATE CHANGE IMPACTS ON CALIFORNIA VEGETATION

    E-Print Network [OSTI]

    CLIMATE CHANGE IMPACTS ON CALIFORNIA VEGETATION: PHYSIOLOGY, LIFE HISTORY, AND ECOSYSTEM CHANGE A White Paper from the California Energy Commission's California Climate Change Center of the uncertainties with climate change effects on terrestrial ecosystems is understanding where transitions

  9. ATNI Tribal Leaders Summit on Climate Change

    Broader source: Energy.gov [DOE]

    The Affiliated Tribes of Northwest Indians is hosting the Tribal Leaders Summit on Climate Change. This two-day conference will discuss climate change impacts, policy on climate change, tribal needs, funding opportunities, and more.

  10. Probabilistic climate change projections using neural networks Received: 30 October 2002 / Accepted: 16 May 2003 / Published online: 5 August 2003

    E-Print Network [OSTI]

    Plattner, Gian-Kasper

    amplify the human impact on the climate system and therefore increase the need for accurate climate projec. This allows us to quantify the effect of the feedback between oceanic and terrestrial carbon uptake and global warming on global temperature projections. Finally, probability density functions for the surface warming

  11. Hydrologic Response to Climate Variability, Climate Change, and Climate Extreme in the U.S.: Climate Model Evaluation and Projections

    SciTech Connect (OSTI)

    Leung, Lai R.; Qian, Yun

    2005-08-01T23:59:59.000Z

    Water resources are sensitive to climate variability and change; predictions of seasonal to interannual climate variations and projections of long-term climate trends can provide significant values in managing water resources. This study examines the control (1975–1995) and future (1995–2100) climate simulated by a global climate model (GCM) and a regional climate simulation driven by the GCM control simulation for the U.S. Comparison of the regional climate simulation with observations across 13 subregions showed that the simulation captured the seasonality and the distributions of precipitation rate quite well. The GCM control and climate change simulations showed that, as a result of a 1% increase in greenhouse gas concentrations per year, there will be a warming of 2–3°C across the U.S. from 2000 to 2100. Although precipitation is not projected to change during this century, the warming trend will increase evapotranspiration to reduce annual basin mean runoff over five subregions along the coastal and south-central U.S.

  12. Climate Dynamics Observational, Theoretical and

    E-Print Network [OSTI]

    Dong, Xiquan

    1 23 Climate Dynamics Observational, Theoretical and Computational Research on the Climate System.6, and -22.5 Wm-2 , respectively, indicating a net cooling effect of clouds on the TOA radiation budget-2 , respectively, resulting in a larger net cooling effect of 2.9 Wm-2 in the model simu- lations

  13. Climatic Change An Interdisciplinary, International

    E-Print Network [OSTI]

    Alvarez, Nadir

    1 23 Climatic Change An Interdisciplinary, International Journal Devoted to the Description, Causes that the most genetically diverse populations are the ones most at risk from climate change, so that global warming will erode the species' genetic variability faster than it curtails the species' geographic

  14. Regional Climate Variability in the Western U.S.: Observed vs. Anticipated

    E-Print Network [OSTI]

    Cycle · ENSO Footprint(s) · Recent Climate Trends · Outlook to Mid-21st Century Range Mgmt. Symposium, Denver, 10 February 10 #12;Average Annual Precipitation for the Western U.S. Based on PRISM OSU/WRCC #12 eruptions, this means more energy input - And higher global temperatures #12;Temperature Widespread warming

  15. The avalanche climate of Glacier National Park, B.C., Canada during 1965-2011

    E-Print Network [OSTI]

    Jamieson, Bruce

    , and rising global average sea levels. It has also been found that the frequency of heavy precipitation events stated that the warming of the climate system is unequivocal, as is now evident from observations of increases in global average air temperature and ocean temperatures, widespread melting of snow and ice

  16. Climate-Change Treaties: A Game-Theoretic Approach Stern School, New York University

    E-Print Network [OSTI]

    Zeeman, Mary Lou

    to global warming, as of 2005. : 1. Average global surface temperatures have risen by 0.6C in the last 140 on as we are, by 2100 global sea levels will probably have risen by 9 to 88cm and average temperatures, 2008 2 / 26 #12;() January 2, 2008 3 / 26 #12;Global warming (or global climate change) is a "tragedy

  17. Contributions of the Atmospheric Radiation Measurement (ARM) Program and the ARM Climate Research Facility to the U.S. Climate Change Science Program

    SciTech Connect (OSTI)

    SA Edgerton; LR Roeder

    2008-09-30T23:59:59.000Z

    The Earth’s surface temperature is determined by the balance between incoming solar radiation and thermal (or infrared) radiation emitted by the Earth back to space. Changes in atmospheric composition, including greenhouse gases, clouds, and aerosols can alter this balance and produce significant climate change. Global climate models (GCMs) are the primary tool for quantifying future climate change; however, there remain significant uncertainties in the GCM treatment of clouds, aerosol, and their effects on the Earth’s energy balance. The 2007 assessment (AR4) by the Intergovernmental Panel on Climate Change (IPCC) reports a substantial range among GCMs in climate sensitivity to greenhouse gas emissions. The largest contributor to this range lies in how different models handle changes in the way clouds absorb or reflect radiative energy in a changing climate (Solomon et al. 2007). In 1989, the U.S. Department of Energy (DOE) Office of Science created the Atmospheric Radiation Measurement (ARM) Program within the Office of Biological and Environmental Research (BER) to address scientific uncertainties related to global climate change, with a specific focus on the crucial role of clouds and their influence on the transfer of radiation in the atmosphere. To address this problem, BER has adopted a unique two-pronged approach: * The ARM Climate Research Facility (ACRF), a scientific user facility for obtaining long-term measurements of radiative fluxes, cloud and aerosol properties, and related atmospheric characteristics in diverse climate regimes. * The ARM Science Program, focused on the analysis of ACRF data to address climate science issues associated with clouds, aerosols, and radiation, and to improve GCMs. This report describes accomplishments of the BER ARM Program toward addressing the primary uncertainties related to climate change prediction as identified by the IPCC.

  18. A 2000 year varve-based climate record from the central Brooks Range, Alaska

    SciTech Connect (OSTI)

    Bird, B.W.; Abbott, M.B.; Finney, B.P.; Kutchko, Barbara

    2009-01-01T23:59:59.000Z

    Varved minerogenic sediments from glacial-fed Blue Lake, northern Alaska, are used to investigate late Holocene climate variability. Varve thickness measurements track summer temperature recorded at Atigun Pass, located 41 km east at a similar elevation (r2 = 0.31, P = 0.08). Results indicate that climate in the Brooks Range from 10 to 730 AD (varve year) was warm with precipitation inferred to be higher than during the twentieth century. The varve-temperature relationship for this period was likely compromised and not used in our temperature reconstruction because the glacier was greatly reduced, or absent, exposing sub-glacial sediments to erosion from enhanced precipitation.

  19. Ecosystem Vulnerability Assessment - Patterns of Climate Change...

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    Ecosystem Vulnerability Assessment - Patterns of Climate Change Vulnerability in the Southwest Ecosystem Vulnerability Assessment - Patterns of Climate Change Vulnerability in the...

  20. Climate VISION: Private Sector Initiatives: Electric Power

    Office of Scientific and Technical Information (OSTI)

    Letters of IntentAgreements The electric power sector participates in the Climate VISION program through the Electric Power Industry Climate Initiative (EPICI) and its Power...

  1. Symbiosis: Addressing Biomass Production Challenges and Climate...

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    Symbiosis: Addressing Biomass Production Challenges and Climate Change Symbiosis: Addressing Biomass Production Challenges and Climate Change This presentation was the opening...

  2. Training for Climate Adaptation in Conservation

    Broader source: Energy.gov [DOE]

    The Wildlife Conservation Society and the Northern Institute of Applied Climate Science are hosting this two-day training for climate adaptation.

  3. Climate VISION: Private Sector Initiatives: Forest Products:...

    Office of Scientific and Technical Information (OSTI)

    agencies, interacting with the legislative branch on climate change issues affecting agriculture and forestry, and representing USDA on U.S. delegations to international climate...

  4. Sandia National Laboratories: Global Climate & Energy

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Rates of Second Key Atmospheric Component On May 1, 2013, in Analysis, Capabilities, Climate, CRF, Energy, Facilities, Global Climate & Energy, Modeling & Analysis, News, News &...

  5. BPA prepares for a changing climate

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    both generally and as part of events such as El Nio. Evidence of global and regional climate change is mounting. The recently released National Climate Assessment confirmed...

  6. Climate VISION: Private Sector Initiatives: Forest Products

    Office of Scientific and Technical Information (OSTI)

    Forest & Paper Association (AF&PA) supports the Climate VISION initiative to address climate change through enhanced research in technology and science, incentives, and...

  7. Projected climate change effects on winterkill in shallow lakes in the northern United States

    SciTech Connect (OSTI)

    Fang, X.; Stefan, H.G.

    2000-03-01T23:59:59.000Z

    Each winter, hundreds of ice-covered, shallow lakes in the northern US are aerated to prevent winterkill, the death of fish due to oxygen depletion under the ice. How will the projected climate warming influence winterkill and the need to artificially aerate lakes? To answer this question, a deterministic, one-dimensional year-round water quality model, which simulates daily dissolved oxygen (DO) profiles and associated water temperatures as well as ice/snow covers on lakes, was applied. Past and projected climate scenarios were investigated. The lake parameters required as model input are surface area, maximum depth, and Secchi depth as a measure of radiation attenuation and trophic state. The model is driven by daily weather data. Weather records from 209 stations in the contiguous US for the period 1961--1979 were used to represent past climate conditions. The projected climate change due to a doubling of atmospheric CO{sub 2} was obtained from the output of the Canadian Climate Center General Circulation Model. To illustrate the effect of projected climate change on lake DO characteristics, the authors present herein DO information simulated, respectively, with inputs of past climate conditions and with a projected 2 x CO{sub 2} climate scenario, as well as differences of those values. Specific parameters obtained were minimum under-ice and lake bottom DO concentration in winter, duration of under-ice anoxic conditions and low DO conditions, and percentage of anoxic and low DO lake volumes during the ice cover period. Under current climate conditions winterkill occurs typically in shallow eutrophic lakes of the northern contiguous US. Climate warming is projected to eliminate winterkill in these lakes. This would be a positive effect of climate warming. Fish species under ice may still experience periods of stress and zero growth due to low DO conditions under projected climate warming.

  8. Overview of different aspects of climate change effects on soils.

    SciTech Connect (OSTI)

    Qafoku, Nikolla

    2014-08-01T23:59:59.000Z

    Climate change [i.e., high atmospheric carbon dioxide (CO2) concentrations (?400 ppm); increasing air temperatures (2-4°C or greater); significant and/or abrupt changes in daily, seasonal, and inter-annual temperature; changes in the wet/dry cycles; intensive rainfall and/or heavy storms; extended periods of drought; extreme frost; heat waves and increased fire frequency] is and will significantly affect soil properties and fertility, water resources, food quantity and quality, and environmental quality. Biotic processes that consume atmospheric CO2 and create organic carbon (C) that is either reprocessed to CO2 or stored in soils, are the subject of active current investigations with great concern over the influence of climate change. In addition, abiotic C cycling and its influence on the inorganic C pool in soils is a fundamental global process in which acidic atmospheric CO2 participates in the weathering of carbonate and silicate minerals, ultimately delivering bicarbonate and Ca2+ or other cations that precipitate in the form of carbonates in soils or are transported to the rivers, lakes, and oceans. Soil responses to climate change will be complex, and there are many uncertainties and unresolved issues. The objective of the review is to initiate and further stimulate a discussion about some important and challenging aspects of climate-change effects on soils, such as accelerated weathering of soil minerals and resulting C and elemental fluxes in and out of soils, soil/geo-engineering methods used to increase C sequestration in soils, soil organic matter (SOM) protection, transformation and mineralization, and SOM temperature sensitivity. This review reports recent discoveries and identifies key research needs required to understand the effects of climate change on soils.

  9. Atmospheric Climate Model Experiments Performed at Multiple Horizontal Resolutions

    SciTech Connect (OSTI)

    Phillips, T; Bala, G; Gleckler, P; Lobell, D; Mirin, A; Maxwell, R; Rotman, D

    2007-12-21T23:59:59.000Z

    This report documents salient features of version 3.3 of the Community Atmosphere Model (CAM3.3) and of three climate simulations in which the resolution of its latitude-longitude grid was systematically increased. For all these simulations of global atmospheric climate during the period 1980-1999, observed monthly ocean surface temperatures and sea ice extents were prescribed according to standard Atmospheric Model Intercomparison Project (AMIP) values. These CAM3.3 resolution experiments served as control runs for subsequent simulations of the climatic effects of agricultural irrigation, the focus of a Laboratory Directed Research and Development (LDRD) project. The CAM3.3 model was able to replicate basic features of the historical climate, although biases in a number of atmospheric variables were evident. Increasing horizontal resolution also generally failed to ameliorate the large-scale errors in most of the climate variables that could be compared with observations. A notable exception was the simulation of precipitation, which incrementally improved with increasing resolution, especially in regions where orography plays a central role in determining the local hydroclimate.

  10. Accelerating development of a predictive science of climate.

    SciTech Connect (OSTI)

    Drake, John B [ORNL; Jones, Phil [Los Alamos National Laboratory (LANL)

    2007-01-01T23:59:59.000Z

    Climate change and studies of its implications are front page news. Could the heat waves of July 2006 in Europe and the US be caused by global warming? Are increased incidences of strong tropical storms and hurricanes like Katrina to be expected? Will coastal cities be flooded due to sea level rise? The National Climatic Data Center (NCDC) which archives all weather data for the nation reports that global surface temperatures have increased at a rate near 0.6 C over the last century but that the trend is three times larger since 1976 [Easterling, 2006]. Will this rate continue or will climate change be even more abrupt? Stepping back from the flurry of questions, scientists must take a systematic approach and develop a predictive framework. With responsibility for advising on energy and technology strategies, the Department of Energy Office of Biological and Environmental Research has chosen to bolster the science of climate in order to get the story straight on the factors that cause climate change and the role of carbon loading from fossil fuel use.

  11. SPRUCE: Spruce and Peatland Responses under Climatic and Environmental Change

    DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

    SPRUCE is an experiment to assess the response of northern peatland ecosystems to increases in temperature and exposures to elevated atmospheric CO2 concentrations. It is the primary component of the Terrestrial Ecosystem Science Scientific Focus Area of ORNL's Climate Change Program, focused on terrestrial ecosystems and the mechanisms that underlie their responses to climatic change. The experimental work is to be conducted in a Picea mariana [black spruce] - Sphagnum spp. bog forest in northern Minnesota, 40 km north of Grand Rapids, in the USDA Forest Service Marcell Experimental Forest (MEF). The site is located at the southern margin of the boreal peatland forest. It is an ecosystem considered especially vulnerable to climate change, and anticipated to be near its tipping point with respect to climate change. Responses to warming and interactions with increased atmospheric CO2 concentration are anticipated to have important feedbacks on the atmosphere and climate, because of the high carbon stocks harbored by such ecosystems.[copied from http://mnspruce.ornl.gov/] While some data files are restricted to access by project members only, others are available for public download now, even as research is being actively conducted.

  12. Some comments on the possible causes of climate change

    E-Print Network [OSTI]

    L. Padget; J. Dunning-Davies

    2008-06-20T23:59:59.000Z

    Climate change is an important current issue and there is much debate about the causes and effects. This article examines the changes in our climate, comparing the recent changes with those in the past. There have been changes in temperature, resulting in an average global rise over the last 300 years, as well as widespread melting of snow and ice, and rising global average sea level. There are many theories for the causes of the recent change in the climate, including some natural and some human influenced. The most widely believed cause of the climate change is increasing levels of Greenhouse gases in the atmosphere and as the atmosphere plays an important role in making our planet inhabitable, it is important to understand it in order to protect it. However, there are other theories for the cause of climate change, the Sun and cosmic rays, for example, are felt by some to have a significant role to play. There is also well-established evidence that the three Milankovitch cycles change the amount and alter the distribution of sunlight over the Earth, heating and cooling it. There are many influences on our planet and they all have differing levels of impact. The purpose of this article is to review the present overall position and urge open, reasoned discussion of the problem.

  13. Mississippi Climate & Hydrology Conference

    SciTech Connect (OSTI)

    Lawford, R.; Huang, J.

    2002-05-01T23:59:59.000Z

    The GEWEX Continental International Project (GCIP), which started in 1995 and completed in 2001, held its grand finale conference in New Orleans, LA in May 2002. Participants at this conference along with the scientists funded through the GCIP program are invited to contribute a paper to a special issue of Journal of Geophysical Research (JGR). This special JGR issue (called GCIP3) will serve as the final report on scientific research conducted by GCIP investigators. Papers are solicited on the following topical areas, but are not limited to, (1) water energy budget studies; (2) warm season precipitation; (3) predictability and prediction system; (4) coupled land-atmosphere models; (5) climate and water resources applications. The research areas cover observations, modeling, process studies and water resources applications.

  14. Modeling the response of plants and ecosystems to elevated CO sub 2 and climate change

    SciTech Connect (OSTI)

    Reynolds, J.F.; Hilbert, D.W.; Chen, Jia-lin; Harley, P.C.; Kemp, P.R.; Leadley, P.W.

    1992-03-01T23:59:59.000Z

    While the exact effects of elevated CO{sub 2} on global climate are unknown, there is a growing consensus among climate modelers that global temperature and precipitation will increase, but that these changes will be non-uniform over the Earth's surface. In addition to these potential climatic changes, CO{sub 2} also directly affects plants via photosynthesis, respiration, and stomatal closure. Global climate change, in concert with these direct effects of CO{sub 2} on plants, could have a significant impact on both natural and agricultural ecosystems. Society's ability to prepare for, and respond to, such changes depends largely on the ability of climate and ecosystem researchers to provide predictions of regional level ecosystem responses with sufficient confidence and adequate lead time.

  15. Modeling the response of plants and ecosystems to elevated CO{sub 2} and climate change

    SciTech Connect (OSTI)

    Reynolds, J.F.; Hilbert, D.W.; Chen, Jia-lin; Harley, P.C.; Kemp, P.R.; Leadley, P.W.

    1992-03-01T23:59:59.000Z

    While the exact effects of elevated CO{sub 2} on global climate are unknown, there is a growing consensus among climate modelers that global temperature and precipitation will increase, but that these changes will be non-uniform over the Earth`s surface. In addition to these potential climatic changes, CO{sub 2} also directly affects plants via photosynthesis, respiration, and stomatal closure. Global climate change, in concert with these direct effects of CO{sub 2} on plants, could have a significant impact on both natural and agricultural ecosystems. Society`s ability to prepare for, and respond to, such changes depends largely on the ability of climate and ecosystem researchers to provide predictions of regional level ecosystem responses with sufficient confidence and adequate lead time.

  16. Lateglacial and early Holocene summer temperatures in the southern Swiss Alps reconstructed using

    E-Print Network [OSTI]

    Bern, Universität

    TINNER1 1 Oeschger Centre for Climate Change Research and Institute of Plant Sciences, University of Bern and of biotic responses to temperature changes throughout Europe and the Mediterranean region. Furthermore our understanding of the long-term dynamics of Mediterranean climate (Tzedakis, 2007

  17. How Do We Know that Human Activities Have Influenced Global Climate?

    SciTech Connect (OSTI)

    Santer, Benjamin D.

    2007-11-05T23:59:59.000Z

    Human activities have significantly altered not only the chemical composition of Earth's atmosphere, but also the climate system. Human influences have led to increases in well-mixed greenhouse gases, decreases in stratospheric ozone, and changes in the atmospheric burdens of sulfate and soot aerosols. All of these atmospheric constituents interact with incoming solar and outgoing terrestrial radiation. Human-induced changes in the concentrations of these constituents modify the natural radiative balance of Earth's atmosphere, and therefore perturb climate. Quantifying the size of the human effect on climate is a difficult statistical problem. 'Fingerprint' methods are typically used for this purpose. These methods involve rigorous statistical comparisons of modeled and observed climate change patterns. Fingerprinting assumes that each individual influence on climate has a unique signature in climate records. The climate fingerprints in response to different forcing factors are typically estimated with computer models, which can be used to perform the controlled experiments that we cannot conduct in the real world. One criticism of the findings of previous scientific assessments is that they have relied heavily on fingerprint studies involving changes in near-surface temperature. Recent fingerprint work, however, has considered a variety of other climate variables, such as ocean heat content, stratospheric temperatures, Northern Hemisphere sea ice extent, sea level pressure, atmospheric water vapor, and the height of the tropopause. These studies illustrate that a human-induced climate change signal is identifiable in many different variables and geographic regions, and that the climate system is telling us an internally- and physically-consistent story.

  18. How Do We Know That Human Activities Have Influenced Global Climate?

    SciTech Connect (OSTI)

    Dr. Benjamin D. Santer

    2007-11-05T23:59:59.000Z

    Human activities have significantly altered not only the chemical composition of Earth's atmosphere, but also the climate system. Human influences have led to increases in well-mixed greenhouse gases, decreases in stratospheric ozone, and changes in the atmospheric burdens of sulfate and soot aerosols. All of these atmospheric constituents interact with incoming solar and outgoing terrestrial radiation. Human-induced changes in the concentrations of these constituents modify the natural radiative balance of Earth's atmosphere, and therefore perturb climate. Quantifying the size of the human effect on climate is a difficult statistical problem. "Fingerprint" methods are typically used for this purpose. These methods involve rigorous statistical comparisons of modeled and observed climate change patterns. Fingerprinting assumes that each individual influence on climate has a unique signature in climate records. The climate fingerprints in response to different forcing factors are typically estimated with computer models, which can be used to perform the controlled experiments that we cannot conduct in the real world. One criticism of the findings of previous scientific assessments is that they have relied heavily on fingerprint studies involving changes in near-surface temperature. Recent fingerprint work, however, has considered a variety of other climate variables, such as ocean heat content, stratospheric temperatures, Northern Hemisphere sea ice extent, sea level pressure, atmospheric water vapor, and the height of the tropopause. These studies illustrate that a human-induced climate change signal is identifiable in many different variables and geographic regions, and that the climate system is telling us an internally- and physically-consistent story.

  19. Forestry and ClimateForestry and Climate ChangeChange

    E-Print Network [OSTI]

    Sheridan, Jennifer

    and Forests:Climate Change and Forests: The GoodThe Good ·Forests as carbon sinks ·Longer growing season · CO2 · Reduced emissions ­ DNR too! · Enhanced sequestration · Bio-energy #12;What to Do?What to Do

  20. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE0 TEMPERATURE

  1. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE0 TEMPERATURE09

  2. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE009 TEMPERATURE

  3. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)1 TEMPERATURE

  4. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)1 TEMPERATURE2

  5. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)1 TEMPERATURE23

  6. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)1 TEMPERATURE234

  7. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)1 TEMPERATURE2345

  8. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)12 TEMPERATURE

  9. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)12 TEMPERATURE3

  10. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)12 TEMPERATURE34

  11. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)12 TEMPERATURE341

  12. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)123 TEMPERATURE

  13. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)123 TEMPERATURE4

  14. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)123 TEMPERATURE41

  15. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)1233 TEMPERATURE

  16. AAA-CLIMATE.XLS

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625 1,006 492 742EnergyOnItemResearch >InternshipDepartmentNeutrino-Induced1 TEMPERATURE (ºF)1233 TEMPERATURE4

  17. Climate Change: The Sun's Role

    E-Print Network [OSTI]

    Gerald E. Marsh

    2007-06-23T23:59:59.000Z

    The sun's role in the earth's recent warming remains controversial even though there is a good deal of evidence to support the thesis that solar variations are a very significant factor in driving climate change both currently and in the past. This precis lays out the background and data needed to understand the basic scientific argument behind the contention that variations in solar output have a significant impact on current changes in climate. It also offers a simple, phenomenological approach for estimating the actual-as opposed to model dependent-magnitude of the sun's influence on climate.

  18. Dalhousie University Climate Change Plan 2010

    E-Print Network [OSTI]

    Brownstone, Rob

    University Climate Change Plan 2010 -- 4 Campus Energy Systems Green Buildings Sustainable TransportDalhousie University Climate Change Plan 2010 #12;Dalhousie University Climate Change Plan 2010 -- 2 The Climate Change Plan was prepared by The Dalhousie Office of Sustainability with advice from

  19. Stormwater, Climate Change and Wisconsin's Coastal Communities

    E-Print Network [OSTI]

    Sheridan, Jennifer

    Stormwater, Climate Change and Wisconsin's Coastal Communities Johnson Foundation at Wingspread · Precipitation and high water · Adapting to our changing climate · Assisting coastal communities Photo: WDNR #12 source of risk from changing climate. City of Green Bay watershed - #12;Predicted climate includes

  20. 2, 11551186, 2006 Mid-Holocene climate

    E-Print Network [OSTI]

    Boyer, Edmond

    CPD 2, 1155­1186, 2006 Mid-Holocene climate change in Europe: a data-model comparison S. Brewer et.clim-past-discuss.net/2/1155/2006/ © Author(s) 2006. This work is licensed under a Creative Commons License. Climate of the Past Discussions Climate of the Past Discussions is the access reviewed discussion forum of Climate

  1. Climate-development-energy policy related seminars

    E-Print Network [OSTI]

    Sussex, University of

    Paula Kivimaa (Finnish Environment Institute) From energy to climate policy in Finland Energy & climate Energy & Climate Tue 3rd Dec 18.00- 19.30 Large Jubilee Jeremy Leggett (SolarCentury) The EnergyClimate-development-energy policy related seminars Autumn term 2013 Date Time Location Speaker

  2. Journal of Climate EARLY ONLINE RELEASE

    E-Print Network [OSTI]

    Hu, Yongyun

    investigate the climate dynamic feedbacks during a transition from the present climate7 to the extremely coldJournal of Climate EARLY ONLINE RELEASE This is a preliminary PDF of the author-produced manuscript. Hu, 2011: The initiation of modern "soft Snowball" and "hard Snowball" climates in CCSM3. Part II

  3. Prospective Climate Change Impact on Large Rivers

    E-Print Network [OSTI]

    Julien, Pierre Y.

    1 Prospective Climate Change Impact on Large Rivers in the US and South Korea Pierre Y. Julien Dept. of Civil and Environ. Eng. Colorado State University Seoul, South Korea August 11, 2009 Climate Change and Large Rivers 1. Climatic changes have been on-going for some time; 2. Climate changes usually predict

  4. An iconic approach to representing climate change

    E-Print Network [OSTI]

    Feigon, Brooke

    1 An iconic approach to representing climate change Saffron Jessica O'Neill A thesis submitted-experts to be meaningfully engaged with the issue of climate change. This thesis investigates the value of engaging non-experts with climate change at the individual level. Research demonstrates that individuals perceive climate change

  5. Climatic Impact of Volcanic Emissions Alan Robock

    E-Print Network [OSTI]

    Robock, Alan

    and interannual climate forecasts following large eruptions, it provides support for nuclear winter theory

  6. Expanding Global Cooperation on Climate Justice

    E-Print Network [OSTI]

    Kammen, Daniel M.

    in evaluating the financial architecture necessary to support just and sustainable climate interventions

  7. Climate impacts on agriculture: Implications for forage and rangeland production

    SciTech Connect (OSTI)

    Izaurralde, Roberto C.; Thomson, Allison M.; Morgan, Jack; Fay, Philip; Polley, Wayne; Hatfield, Jerry L.

    2011-04-19T23:59:59.000Z

    Projections of temperature and precipitation patterns across the United States during the next 50 years anticipate a 1.5 to 2°C warming and a slight increase in precipitation as a result of global climate change. There have been relatively few studies of climate change impacts on pasture and rangeland (grazingland) species compared to those on crop species, despite the economic and ecological importance of the former. Here we review the literature on pastureland and rangeland species to rising CO2 and climate change (temperature, and precipitation) and discuss plant and management factors likely to influence pastureland and rangeland responses to change (e.g., community composition, plant competition, perennial growth habit, seasonal productivity, and management methods). Overall, the response of pasture species to increased [CO2] is consistent with the general response of C3 and C4 type vegetation, although significant exceptions exist. Both pastureland and rangeland species should exhibit an acceleration of metabolism and development due to earlier onset of spring green-up and longer growing seasons. However, in the studies reviewed here, C3 pasture species increased their photosynthetic rates by up to 40% while C4 species exhibited no increase in photosynthesis. In general, it is expected that increases in [CO2] and precipitation would enhance rangeland net primary production (NPP) while increased air temperatures would either increase or decrease NPP. Much of this uncertainty in response is due to uncertain future projections of precipitation, both globally and regionally. For example, if annual precipitation changes little or declines, rangeland plant response to warming temperatures and rising [CO2] may be neutral or may decline due to increased water stress. This review reveals the need for comprehensive studies of climate change impacts on the pasture ecosystem including grazing regimes, mutualistic relationships (e.g., plant roots-nematodes; N-fixing organisms), as well as the ecosystem carbon balance, essential nutrients, and water.

  8. Studies of dynamical processes affecting global climate

    SciTech Connect (OSTI)

    Keller, C.; Cooper, D.; Eichinger, W. [and others

    1998-12-31T23:59:59.000Z

    This is the final report of a three-year, Laboratory Directed Research and Development project at the Los Alamos National Laboratory (LANL). The main objective was, by a combined theoretical and observational approach, to develop improved models of dynamic processes in the oceans and atmosphere and to incorporate them into large climate codes, chiefly in four main areas: numerical physics, chemistry, water vapor, and ocean-atmosphere interactions. Main areas of investigation included studies of: cloud parameterizations for global climate codes, Lidar and the planetary boundary layer, chemistry, climate variability using coupled ocean-atmospheric models, and numerical physical methods. This project employed a unique approach that included participation of a number of University of California faculty, postdoctoral fellows and graduate students who collaborated with Los Alamos research staff on specific tasks, thus greatly enhancing the research output. Overall accomplishments during the sensing of the atmospheric planetary were: (1) first two- and three-dimensional remote sensing of the atmospheric planetary boundary layer using Lidars, (2) modeling of 20-year cycle in both pressure and sea surface temperatures in North Pacific, (3) modeling of low frequency internal variability, (4) addition of aerosols to stratosphere to simulate Pinatubo effect on ozone, (5) development of fast, comprehensive chemistry in the troposphere for urban pollution studies, (6) new prognostic cloud parameterization in global atmospheric code remedied problems with North Pacific atmospheric circulation and excessive equatorial precipitation, (7) development of a unique aerosol analysis technique, the aerosol time-of-flight mass spectrometer (ATOFMS), which allows real-time analysis of the size and chemical composition of individual aerosol particles, and (8) numerical physics applying Approximate Inertial Manifolds to ocean circulation. 14 refs., 6 figs.

  9. Watershed response and land energy feedbacks under climate change depend upon groundwater.

    SciTech Connect (OSTI)

    Maxwell, R M; Kollet, S J

    2008-06-10T23:59:59.000Z

    Human induced climate change will have a significant impact on the hydrologic cycle, creating changes in fresh water resources, land cover, and feedbacks that are difficult to characterize, which makes it an issue of global importance. Previous studies have not included subsurface storage in climate change simulations and feedbacks. A variably-saturated groundwater flow model with integrated overland flow and land surface model processes is used to examine the interplay between coupled water and energy processes under climate change conditions. A case study from the Southern Great Plains (SGP) USA, an important agricultural region that is susceptible to drought, is used as the basis for three scenarios simulations using a modified atmospheric forcing dataset to reflect predicted effects due to human-induced climate change. These scenarios include an increase in the atmospheric temperature and variations in rainfall amount and are compared to the present-day climate case. Changes in shallow soil saturation and groundwater levels are quantified as well as the corresponding energy fluxes at the land surface. Here we show that groundwater and subsurface lateral flow processes are critical in understanding hydrologic response and energy feedbacks to climate change and that certain regions are more susceptible to changes in temperature, while others to changes in precipitation. This groundwater control is critical for understanding recharge and drought processes, possible under future climate conditions.

  10. Climate Insights 101 Questions and Discussion Points: Module 1, Lesson 4: An Introduction to Climate Modelling

    E-Print Network [OSTI]

    Pedersen, Tom

    Climate Insights 101 Questions and Discussion Points: Module 1, Lesson 4: An Introduction to Climate Modelling 1 Climate Insights 101 Questions and Discussion Points Module 1, Lesson 4: An Introduction to Climate Modelling Available at http://pics.uvic.ca/education/climate-insights-101 Updated May

  11. Climate Sensitivity Estimated From Earth's Climate History James E. Hansen and Makiko Sato

    E-Print Network [OSTI]

    Hansen, James E.

    1 Climate Sensitivity Estimated From Earth's Climate History James E. Hansen and Makiko Sato NASA's climate history potentially can yield accurate assessment of climate sensitivity. Imprecise knowledge of the fast-feedback climate sensitivity, which is the sensitivity that most immediately affects humanity. Our

  12. Chicago Climate Exchange, Inc. 2010 Chicago Climate Exchange 1 The Role of Exchanges and Standardization

    E-Print Network [OSTI]

    Chicago Climate Exchange®, Inc.© 2010 Chicago Climate Exchange 1 The Role of Exchanges and Standardization in Reducing Emissions at Scale Michael J. Walsh, Ph.D. Executive Vice President Chicago Climate Exchange, Inc. #12;Chicago Climate Exchange®, Inc.© 2010 Chicago Climate Exchange Pacala-Socolow GHG

  13. Climate Mathematician Job Advertisement, September 2013 FACULTY POSITION IN CLIMATE MATHEMATICS

    E-Print Network [OSTI]

    Gallo, Linda C.

    1 Climate Mathematician Job Advertisement, September 2013 FACULTY POSITION IN CLIMATE MATHEMATICS in Climate Mathematics, beginning in August 2014. Exceptional candidates at the Associate Professor level an active interdisciplinary research program in climate mathematics with a focus on next generation climate

  14. "Climate change is sure to occur in some form." The study of climate impacts notes

    E-Print Network [OSTI]

    "Climate change is sure to occur in some form." 1 #12;The study of climate impacts notes how scientists generally agree that humans are changing the climate, and that if we continue pumping carbon we learn from past climate variations? How can we best adapt to climate change? This report attempts

  15. Global Climate Change,Global Climate Change, Land Cover Change, andLand Cover Change, and

    E-Print Network [OSTI]

    1 Global Climate Change,Global Climate Change, Land Cover Change, andLand Cover Change Changes · Due to ­ Climate Change ­ Land Cover / Land Use Change ­ Interaction of Climate and Land Cover Change · Resolution ­ Space ­ Time Hydro-Climatic Change · Variability vs. Change (Trends) · Point data

  16. Assessing the effects of ocean diffusivity and climate sensitivity on the rate of global climate change

    E-Print Network [OSTI]

    Schmittner, Andreas

    sensitivity and ocean heat uptake on the rate of future climate change. We apply a range of values for climate a significant effect on the rate of transient climate change for high values of climate sensitivity, while values of climate sensitivity and low values of ocean diffusivity. Such high rates of change could

  17. Free and forced tropical variability: role of the wind-evaporation-sea surface temperature (WES) feedback

    E-Print Network [OSTI]

    Mahajan, Salil

    2009-05-15T23:59:59.000Z

    The Wind-Evaporation-Sea Surface Temperature (WES) feedback is believedto play an important role in the tropics, where climate variability is governed byatmosphere-ocean coupled interactions. This dissertation reports on studies to distinctlyisolate...

  18. Nature Climate Change features Los

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Climate Change features Los Alamos forest research February 27, 2013 New print edition of journal tags tree-stress project for cover story LOS ALAMOS, N.M., Feb. 27, 2013-The print...

  19. Climate Action Plan (New Jersey)

    Broader source: Energy.gov [DOE]

    The NJDEP Office of Sustainability and Green Energy coordinates programs that reduce greenhouse gas emissions that cause climate change, as well as programs designed to help New Jersey become...

  20. Electric Vehicles Global Climate Change

    E-Print Network [OSTI]

    Sóbester, András

    Hot Topics Electric Vehicles Global Climate Change Green Building Hydraulic Fracturing Nuclear to global warming. The UKgovernment has just announced it is investing $1 billion in their development Green Living Industry Regulation Remediation Research and Technology Sustainability Waste Water Products

  1. Climate sensitivity of marine energy 

    E-Print Network [OSTI]

    Harrison, Gareth P; Wallace, Robin

    2005-01-01T23:59:59.000Z

    Marine energy has a significant role to play in lowering carbon emissions within the energy sector. Paradoxically, it may be susceptible to changes in climate that will result from rising carbon emissions. Wind patterns are expected to change...

  2. Essays in climate and development

    E-Print Network [OSTI]

    Guerrero Compeán, Roberto

    2013-01-01T23:59:59.000Z

    This dissertation is a collection of three essays on environmental policy and empirical development economics, unified in their underlying inquiry of the welfare effects of climate in Mexico. The first chapter presents ...

  3. Climate Action Plan (North Carolina)

    Broader source: Energy.gov [DOE]

    The North Carolina Department of Environmental and Natural Resources (DENR) has established a priority in the 2009 - 2013 Strategic Plan to respond to climate change using both mitigation and...

  4. Tropical Cyclones and Climate Change

    E-Print Network [OSTI]

    Knutson, Thomas R.

    Whether the characteristics of tropical cyclones have changed or will change in a warming climate — and if so, how — has been the subject of considerable investigation, often with conflicting results. Large amplitude ...

  5. 2009 Operations Employee Climate Survey

    E-Print Network [OSTI]

    2009 Operations Employee Climate Survey March 2009 #12;Acknowledgements TheBerkeleyLab Survey Team Associates has conducted a number of large-scale surveys for organizations in higher education, including MIT. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3 Survey

  6. Climate change and water supply, management and use: A literature review

    SciTech Connect (OSTI)

    Chang, L.H.; Draves, J.D.; Hunsaker, C.T.

    1992-05-01T23:59:59.000Z

    There is evidence that atmospheric concentrations Of C0{sub 2}, tropospheric 0{sub 3}, and CH{sub 4}, among other gases that contribute to the greenhouse effect, have increased in recent decades, and that these changes may induce changes in global air temperatures and regional climate features in coming years. A literature review was conducted to sample the literature base on which our understanding of the water resource impacts of climate change rests. Water resource issues likely to be important include hydrologic response to climate change, the resilience of water supply systems to changing climatic and hydrologic conditions, and the effects of climate change on water quality and water uses (such as navigation and energy generation). A computer-assisted search of literature on the effects of climate change on these subjects was conducted. All studies were classified by type of paper (e.g., review, discussion, case study), region, water resource variable studied, and source of climate scenario. The resulting bibliography containing more than 200 references was largely annotated. Case studies of potential hydrologic impacts have been more common than studies of impacts on water management or water use, but this apparent research gap is decreasing. Case studies demonstrating methods of incorporating potential risks of climate change into water project planning and management have been performed. Considerable variability in regional coverage exists; the Great Lakes basin and California receive relatively more attention than such regions as New England and the Missouri River basin. General circulation model-based and hypothetical climate scenarios have been the dominant sources of climate scenarios used in case studies, although a variety of other methods for developing climate scenarios have been developed.

  7. Glossary: Carbon dioxide and climate

    SciTech Connect (OSTI)

    Not Available

    1990-08-01T23:59:59.000Z

    This Glossary contains definitions of selected CO{sub 2}-related terms as well as tables containing information related to CO{sub 2} and climate. Each term is defined with an emphasis on its relationship to CO{sub 2} and climate. Many of the definitions are then followed by a more detailed description of the term and its use. References to the literature from which the definitions were taken are listed at the end of the Glossary.

  8. High Temperatures & Electricity Demand

    E-Print Network [OSTI]

    High Temperatures & Electricity Demand An Assessment of Supply Adequacy in California Trends.......................................................................................................1 HIGH TEMPERATURES AND ELECTRICITY DEMAND.....................................................................................................................7 SECTION I: HIGH TEMPERATURES AND ELECTRICITY DEMAND ..........................9 BACKGROUND

  9. www.climate.iitb.ac.in 1st CLIMATE SCIENCE AND

    E-Print Network [OSTI]

    Sarawagi, Sunita

    and emissions modeling, Climate mitigation technologies (enhanced carbon capture systems, photoactive materials and technology: Terrestrial carbon sources and sinks, Prediction of climate extremes, Climate perturbation and devices, non-carbon energy technologies, biorefineries, negative net-carbon technologies

  10. Internalizing Climate Change—Scientific Resource Management and the Climate Change Challenges

    E-Print Network [OSTI]

    Dettinger, Michael D.; Culberson, Steven

    2008-01-01T23:59:59.000Z

    Council. 2001. Climate change sci- ence: an analysis of someNWT, Dracup JA. 2004. Climate change impacts uncertainty forVR, Kusler J. 2000. Climate change: Potential impacts and

  11. The Community Climate System Model Version 4

    SciTech Connect (OSTI)

    Gent, Peter R.; Danabasoglu, Gokhan; Donner, Leo J.; Holland, Marika M.; Hunke, Elizabeth C.; Jayne, Steve R.; Lawrence, David M.; Neale, Richard; Rasch, Philip J.; Vertenstein, Mariana; Worley, Patrick; Yang, Zong-Liang; Zhang, Minghua

    2011-10-01T23:59:59.000Z

    The fourth version of the Community Climate System Model (CCSM4) was recently completed and released to the climate community. This paper describes developments to all the CCSM components, and documents fully coupled pre-industrial control runs compared to the previous version, CCSM3. Using the standard atmosphere and land resolution of 1{sup o} results in the sea surface temperature biases in the major upwelling regions being comparable to the 1.4{sup o} resolution CCSM3. Two changes to the deep convection scheme in the atmosphere component result in the CCSM4 producing El Nino/Southern Oscillation variability with a much more realistic frequency distribution than the CCSM3, although the amplitude is too large compared to observations. They also improve the representation of the Madden-Julian Oscillation, and the frequency distribution of tropical precipitation. A new overflow parameterization in the ocean component leads to an improved simulation of the deep ocean density structure, especially in the North Atlantic. Changes to the CCSM4 land component lead to a much improved annual cycle of water storage, especially in the tropics. The CCSM4 sea ice component uses much more realistic albedos than the CCSM3, and the Arctic sea ice concentration is improved in the CCSM4. An ensemble of 20th century simulations runs produce an excellent match to the observed September Arctic sea ice extent from 1979 to 2005. The CCSM4 ensemble mean increase in globally-averaged surface temperature between 1850 and 2005 is larger than the observed increase by about 0.4 C. This is consistent with the fact that the CCSM4 does not include a representation of the indirect effects of aerosols, although other factors may come into play. The CCSM4 still has significant biases, such as the mean precipitation distribution in the tropical Pacific Ocean, too much low cloud in the Arctic, and the latitudinal distributions of short-wave and long-wave cloud forcings.

  12. Estimating present climate in a warming world: a model-based approach

    SciTech Connect (OSTI)

    Raeisaenen, J.; Ruokolainen, L. [University of Helsinki (Finland). Division of Atmospheric Sciences and Geophysics

    2008-09-30T23:59:59.000Z

    Weather services base their operational definitions of 'present' climate on past observations, using a 30-year normal period such as 1961-1990 or 1971-2000. In a world with ongoing global warming, however, past data give a biased estimate of the actual present-day climate. Here we propose to correct this bias with a 'delta change' method, in which model-simulated climate changes and observed global mean temperature changes are used to extrapolate past observations forward in time, to make them representative of present or future climate conditions. In a hindcast test for the years 1991-2002, the method works well for temperature, with a clear improvement in verification statistics compared to the case in which the hindcast is formed directly from the observations for 1961-1990. However, no improvement is found for precipitation, for which the signal-to-noise ratio between expected anthropogenic changes and interannual variability is much lower than for temperature. An application of the method to the present (around the year 2007) climate suggests that, as a geographical average over land areas excluding Antarctica, 8-9 months per year and 8-9 years per decade can be expected to be warmer than the median for 1971-2000. Along with the overall warming, a substantial increase in the frequency of warm extremes at the expense of cold extremes of monthly-to-annual temperature is expected.

  13. Climate change risk and response

    E-Print Network [OSTI]

    Kahrl, Fredrich; Roland-Holst, David

    2008-01-01T23:59:59.000Z

    cooling. For California’s dairy cows, higher body temperatures mean lower milkcooling. California dairy cows are particularly vulnerable because higher temperatures mean less milk.

  14. President Obama on Climate Change | Department of Energy

    Broader source: Energy.gov (indexed) [DOE]

    President Obama on Climate Change President Obama on Climate Change Addthis Speakers President Barack Obama Duration 2:46 Topic Energy Sector Jobs Renewables Solar Climate Change...

  15. Climate Change, the Clean Air Act, and Industrial Pollution

    E-Print Network [OSTI]

    Kaswan, Alice

    2012-01-01T23:59:59.000Z

    Climate Change, the Clean Air Act, and Industrial PollutionCONSIDERATIONS IN CLIMATE POLICY . A.pollutant Considerations into Climate Policy 1.

  16. Climate Change and San Francisco Bay-Delta Tidal Wetlands

    E-Print Network [OSTI]

    Parker, V. Thomas; Callaway, John C.; Schile, Lisa M.; Vasey, Michael C.; Herbert, Ellen R.

    2011-01-01T23:59:59.000Z

    National Institute for Climate Change Research, Coastalthe context of predicted climate change. Madroño 54(3):234–18–20. Dettinger MD. 2005. From climate-change spaghetti to

  17. Supercomputers Fuel Global High-Resolution Climate Models

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    Supercomputers Fuel Global High-Resolution Climate Models Supercomputers Fuel Global High-Resolution Climate Models Berkeley Lab Researcher Says Climate Science is Entering New...

  18. Building Science-Based Climate Maps - Building America Top Innovation...

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    Science-Based Climate Maps - Building America Top Innovation Building Science-Based Climate Maps - Building America Top Innovation Photo showing climate zone maps based on the IECC...

  19. Building America Climate-Specific Guidance | Department of Energy

    Energy Savers [EERE]

    Building America Building America Climate-Specific Guidance Building America Climate-Specific Guidance Building America Climate-Specific Guidance 2014 Housing Innovation...

  20. Stakeholder Engagement in Climate Change Policymaking in American Cities

    E-Print Network [OSTI]

    Fiack, Duran; Kamieniecki , Sheldon

    2015-01-01T23:59:59.000Z

    the dimensions of climate change communication by conductingdynamics around climate change communication at thethe dimensions of climate change communication by conducting

  1. Economic Damages from Climate Change: An Assessment of Market Impacts

    E-Print Network [OSTI]

    Hanemann, W Michael; Dale, Larry

    2006-01-01T23:59:59.000Z

    the affects of climate change on agriculture in irrigatedmarket impacts from climate change on US agriculture and onimpacts of climate change on US agriculture. The first set

  2. Seawalls Are Not Enough: Climate Change & U.S. Interests

    E-Print Network [OSTI]

    Freeman, Jody; Guzman, Andrew

    2009-01-01T23:59:59.000Z

    The impact of climate change on agriculture, for example, isthe impacts of climate change on agriculture. The reasonsimpact of climate change on agriculture, forestry, coastal

  3. Northeast Climate Science Center: Transposing Extreme Rainfall to Assess Climate Vulnerability

    Office of Energy Efficiency and Renewable Energy (EERE)

    Climate models predict significant increases in the magnitude and frequency of extreme rainfalls.  However, climate model projections of precipitation vary greatly across models.  For communities...

  4. Global Warming What is Climate? Ocean's Role in Climate Change Uncertainty Quantification, the Next Frontier The Role Played by Oceans in Climate

    E-Print Network [OSTI]

    Restrepo, Juan M.

    Global Warming What is Climate? Ocean's Role in Climate Change Uncertainty Quantification, the Next Department University of Arizona October 11, 2008 #12;Global Warming What is Climate? Ocean's Role in Climate, Undergraduate Students: 2. UQGQG #12;Global Warming What is Climate? Ocean's Role in Climate Change Uncertainty

  5. AEROSOL, CLOUDS, AND CLIMATE CHANGE

    SciTech Connect (OSTI)

    SCHWARTZ, S.E.

    2005-09-01T23:59:59.000Z

    Earth's climate is thought to be quite sensitive to changes in radiative fluxes that are quite small in absolute magnitude, a few watts per square meter, and in relation to these fluxes in the natural climate. Atmospheric aerosol particles exert influence on climate directly, by scattering and absorbing radiation, and indirectly by modifying the microphysical properties of clouds and in turn their radiative effects and hydrology. The forcing of climate change by these indirect effects is thought to be quite substantial relative to forcing by incremental concentrations of greenhouse gases, but highly uncertain. Quantification of aerosol indirect forcing by satellite- or ground-based remote sensing has proved quite difficult in view of inherent large variation in the pertinent observables such as cloud optical depth, which is controlled mainly by liquid water path and only secondarily by aerosols. Limited work has shown instances of large magnitude of aerosol indirect forcing, with local instantaneous forcing upwards of 50 W m{sup 66}-2. Ultimately it will be necessary to represent aerosol indirect effects in climate models to accurately identify the anthropogenic forcing at present and over secular time and to assess the influence of this forcing in the context of other forcings of climate change. While the elements of aerosol processes that must be represented in models describing the evolution and properties of aerosol particles that serve as cloud condensation particles are known, many important components of these processes remain to be understood and to be represented in models, and the models evaluated against observation, before such model-based representations can confidently be used to represent aerosol indirect effects in climate models.

  6. Regional Climate Modeling: Progress, Challenges, and Prospects

    SciTech Connect (OSTI)

    Wang, Yuqing; Leung, Lai R.; McGregor, John L.; Lee, Dong-Kyou; Wang, Wei-Chyung; Ding, Yihui; Kimura, Fujio

    2004-12-01T23:59:59.000Z

    Regional climate modeling with regional climate models (RCMs) has matured over the past decade and allows for meaningful utilization in a broad spectrum of applications. In this paper, latest progresses in regional climate modeling studies are reviewed, including RCM development, applications of RCMs to dynamical downscaling for climate change assessment, seasonal climate predictions and climate process studies, and the study of regional climate predictability. Challenges and potential directions of future research in this important area are discussed, with the focus on those to which less attention has been given previously, such as the importance of ensemble simulations, further development and improvement of regional climate modeling approach, modeling extreme climate events and sub-daily variation of clouds and precipitation, model evaluation and diagnostics, applications of RCMs to climate process studies and seasonal predictions, and development of regional earth system models. It is believed that with both the demonstrated credibility of RCMs’ capability in reproducing not only monthly to seasonal mean climate and interannual variability but also the extreme climate events when driven by good quality reanalysis and the continuous improvements in the skill of global general circulation models (GCMs) in simulating large-scale atmospheric circulation, regional climate modeling will remain an important dynamical downscaling tool for providing the needed information for assessing climate change impacts and seasonal climate predictions, and a powerful tool for improving our understanding of regional climate processes. An internationally coordinated effort can be developed with different focuses by different groups to advance regional climate modeling studies. It is also recognized that since the final quality of the results from nested RCMs depends in part on the realism of the large-scale forcing provided by GCMs, the reduction of errors and improvement in physics parameterizations in both GCMs and RCMs remain a priority for climate modeling community.

  7. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE (ºF) (3-FT

  8. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE (ºF) (3-FT09

  9. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE (ºF)

  10. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE (ºF)09

  11. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE (ºF)0910

  12. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE (ºF)091009

  13. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE (ºF)09100910

  14. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE

  15. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE0

  16. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE009

  17. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE00909

  18. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE0090910

  19. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative1 First Use of Energy for All Purposes (Fuel and Nonfuel), 2002; Level: National5Sales for4,645 3,625govInstrumentstdmadapInactiveVisiting the TWPSuccessAlamosCharacterization2 PermitClean0 TEMPERATURE009091009

  20. Climat.xls

    Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

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  1. AAA-CLIMATE.XLS

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  2. AAA-CLIMATE.XLS

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  3. AAA-CLIMATE.XLS

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  4. AAA-CLIMATE.XLS

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  5. AAA-CLIMATE.XLS

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  6. AAA-CLIMATE.XLS

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  7. AAA-CLIMATE.XLS

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  8. AAA-CLIMATE.XLS

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  9. AAA-CLIMATE.XLS

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  10. AAA-CLIMATE.XLS

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  11. AAA-CLIMATE.XLS

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  12. AAA-CLIMATE.XLS

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  13. AAA-CLIMATE.XLS

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  14. AAA-CLIMATE.XLS

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  15. AAA-CLIMATE.XLS

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  16. AAA-CLIMATE.XLS

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  17. AAA-CLIMATE.XLS

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  18. AAA-CLIMATE.XLS

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  19. AAA-CLIMATE.XLS

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  20. AAA-CLIMATE.XLS

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  1. AAA-CLIMATE.XLS

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  2. AAA-CLIMATE.XLS

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  3. AAA-CLIMATE.XLS

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  4. AAA-CLIMATE.XLS

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  5. AAA-CLIMATE.XLS

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  6. Climate-Soil-Vegetation Control on Groundwater Table Dynamics and its Feedbacks in a Climate Model

    SciTech Connect (OSTI)

    Leung, Lai-Yung R.; Huang, Maoyi; Qian, Yun; Liang, Xu

    2010-01-29T23:59:59.000Z

    Among the three dynamically linked branches of the water cycle, including atmospheric, surface, and subsurface water, groundwater is the largest reservoir and an active component of the hydrologic system. Because of the inherent slow response time, groundwater may be particularly relevant for long time-scale processes such as multi-years or decadal droughts. This study uses regional climate simulations with and without surface water – groundwater interactions for the conterminous U.S. to assess the influence of climate, soil, and vegetation on groundwater table dynamics, and its potential feedbacks to regional climate. Analysis shows that precipitation has a dominant influence on the spatial and temporal variations of groundwater table depth (GWT). The simulated GWT is found to decrease sharply with increasing precipitation. Our simulation also shows some distinct spatial variations that are related to soil porosity and hydraulic conductivity. Vegetation properties such as minimum stomatal resistance, and root depth and fraction are also found to play an important role in controlling the groundwater table. Comparing two simulations with and without groundwater table dynamics, we find that groundwater table dynamics mainly influences the partitioning of soil water between the surface (0 – 0.5 m) and subsurface (0.5 – 5 m) rather than total soil moisture. In most areas, groundwater table dynamics increases surface soil moisture at the expense of the subsurface, except in regions with very shallow groundwater table. The change in soil water partitioning between the surface and subsurface is found to strongly correlate with the partitioning of surface sensible and latent heat fluxes. The evaporative fraction (EF) is generally higher during summer when groundwater table dynamics is included. This is accompanied by increased cloudiness, reduced diurnal temperature range, cooler surface temperature, and increased cloud top height. Although both convective and non-convective precipitation are enhanced, the higher EF changes the partitioning to favor more non-convective precipitation, but this result could be sensitive to the convective parameterization used. Compared to simulations without groundwater table dynamics, the dry bias in the summer precipitation is slightly reduced over the central and eastern U.S. Groundwater table dynamics can provide important feedbacks to atmospheric processes, and these feedbacks are stronger in regions with deeper groundwater table, because the interactions between surface and subsurface are weak when the groundwater table is deep. This increases the sensitivity of surface soil moisture to precipitation anomalies, and therefore enhances land surface feedbacks to the atmosphere through changes in soil moisture and evaporative fraction. By altering the groundwater table depth, land use change and groundwater withdrawal can alter land surface response and feedback to the climate system.

  7. A National Strategy for Advancing Climate Modeling

    SciTech Connect (OSTI)

    Dunlea, Edward; Elfring, Chris

    2012-12-04T23:59:59.000Z

    Climate models are the foundation for understanding and projecting climate and climate-related changes and are thus critical tools for supporting climate-related decision making. This study developed a holistic strategy for improving the nationâ??s capability to accurately simulate climate and related Earth system changes on decadal to centennial timescales. The committeeâ??s report is a high level analysis, providing a strategic framework to guide progress in the nationâ??s climate modeling enterprise over the next 10-20 years. This study was supported by DOE, NSF, NASA, NOAA, and the intelligence community.

  8. Earths Climate Sensitivity: Apparent Inconsistencies in Recent Assessments

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Schwartz, Stephen E.; Charlson, Robert J.; Kahn, Ralph; Rodhe, Henning

    2014-12-01T23:59:59.000Z

    Earth's equilibrium climate sensitivity (ECS) and forcing of Earth's climate system over the industrial era have been re-examined in two new assessments: the Fifth Assessment Report (AR5) of the Intergovernmental Panel on Climate Change (IPCC), and a study by Otto et al. (2013). The ranges of these quantities given in these assessments and also in the Fourth (2007) IPCC Assessment are analyzed here within the framework of a planetary energy balance model, taking into account the observed increase in global mean surface temperature over the instrumental record together with best estimates of the rate of increase of planetary heat content.more »This analysis shows systematic differences among the several assessments and apparent inconsistencies within individual assessments. Importantly, the likely range of ECS to doubled CO? given in AR5, 1.5–4.5 K/(3.7 W m?²) exceeds the range inferred from the assessed likely range of forcing, 1.2–2.9 K/(3.7 W m?²), where 3.7 W ?² denotes the forcing for doubled CO?. Such differences underscore the need to identify their causes and reduce the underlying uncertainties. Explanations might involve underestimated negative aerosol forcing, overestimated total forcing, overestimated climate sensitivity, poorly constrained ocean heating, limitations of the energy balance model, or a combination of effects.« less

  9. Earths Climate Sensitivity: Apparent Inconsistencies in Recent Assessments

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Schwartz, Stephen E. [Brookhaven National Laboratory (BNL), Upton, NY (United States); Charlson, Robert J. [Univ. of Washington, Seattle, WA (United States); Kahn, Ralph [NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States); Rodhe, Henning [Stockholm Univ. (Sweden)

    2014-12-01T23:59:59.000Z

    Earth's equilibrium climate sensitivity (ECS) and forcing of Earth's climate system over the industrial era have been re-examined in two new assessments: the Fifth Assessment Report (AR5) of the Intergovernmental Panel on Climate Change (IPCC), and a study by Otto et al. (2013). The ranges of these quantities given in these assessments and also in the Fourth (2007) IPCC Assessment are analyzed here within the framework of a planetary energy balance model, taking into account the observed increase in global mean surface temperature over the instrumental record together with best estimates of the rate of increase of planetary heat content. This analysis shows systematic differences among the several assessments and apparent inconsistencies within individual assessments. Importantly, the likely range of ECS to doubled CO? given in AR5, 1.5–4.5 K/(3.7 W m?²) exceeds the range inferred from the assessed likely range of forcing, 1.2–2.9 K/(3.7 W m?²), where 3.7 W ?² denotes the forcing for doubled CO?. Such differences underscore the need to identify their causes and reduce the underlying uncertainties. Explanations might involve underestimated negative aerosol forcing, overestimated total forcing, overestimated climate sensitivity, poorly constrained ocean heating, limitations of the energy balance model, or a combination of effects.

  10. Economics, ethics, and climate policy

    SciTech Connect (OSTI)

    Howarth, R.B.; Monahan, P.A.

    1992-11-01T23:59:59.000Z

    Are the costs of greenhouse gas emissions abatement justified by the perceived benefits of sustained climate stability Do people of the present generation have a moral right to impose climate risks on their descendants in generations to come This report examines these questions in light of the emergent facts of climate science and their socioeconomic implications. We consider alternative normative criteria for social decision-making with particular emphasis on cost-benefit analysis and the principle of sustainable development. While each framework yields important insights, we argue that the gross uncertainties associated with climate change and the distribution of impacts between present and future generations constrain the usefulness of cost-benefit criteria in evaluating climate policy. If one accepts the ethical proposition that it is morally wrong to impose catastrophic risks on unborn generations when reducing those risks would not noticeably diminish the quality of life of existing persons, a case can be made for concerted policy action to reduce greenhouse gas emissions.

  11. Economics, ethics, and climate policy

    SciTech Connect (OSTI)

    Howarth, R.B.; Monahan, P.A.

    1992-11-01T23:59:59.000Z

    Are the costs of greenhouse gas emissions abatement justified by the perceived benefits of sustained climate stability? Do people of the present generation have a moral right to impose climate risks on their descendants in generations to come? This report examines these questions in light of the emergent facts of climate science and their socioeconomic implications. We consider alternative normative criteria for social decision-making with particular emphasis on cost-benefit analysis and the principle of sustainable development. While each framework yields important insights, we argue that the gross uncertainties associated with climate change and the distribution of impacts between present and future generations constrain the usefulness of cost-benefit criteria in evaluating climate policy. If one accepts the ethical proposition that it is morally wrong to impose catastrophic risks on unborn generations when reducing those risks would not noticeably diminish the quality of life of existing persons, a case can be made for concerted policy action to reduce greenhouse gas emissions.

  12. The AmeriFlux Data Activity and Data System: An Evolving Collection of Data Management Techniques, Tools, Products and Services

    SciTech Connect (OSTI)

    Boden, Thomas A [ORNL; Krassovski, Misha B [ORNL; Yang, Bai [ORNL

    2013-01-01T23:59:59.000Z

    The Carbon Dioxide Information Analysis Center (CDIAC) at Oak Ridge National Laboratory (ORNL), USA has provided scientific data management support for the U.S. Department of Energy and international climate change science since 1982. Over this period, climate change science has expanded from research focusing on basic understanding of geochemical cycles, particularly the carbon cycle, to integrated research addressing climate change impacts, vulnerability, adaptation, and mitigation. Interests in climate change data and information worldwide have grown remarkably and, as a result, so have demands and expectations for CDIAC s data systems. To meet the growing demands, CDIAC s strategy has been to design flexible data systems using proven technologies blended with new, evolving technologies and standards. CDIAC development teams are multidisciplinary and include computer science and information technology expertise, but also scientific expertise necessary to address data quality and documentation issues and to identify data products and system capabilities needed by climate change scientists. CDIAC has learned there is rarely a single commercial tool or product readily available to satisfy long-term scientific data system requirements (i.e., one size does not fit all and the breadth and diversity of environmental data are often too complex for easy use with commercial products) and typically deploys a variety of tools and data products in an effort to provide credible data freely to users worldwide. Like many scientific data management applications, CDIAC s data systems are highly customized to satisfy specific scientific usage requirements (e.g., developing data products specific for model use) but are also designed to be flexible and interoperable to take advantage of new software engineering techniques, standards (e.g., metadata standards) and tools and to support future Earth system data efforts (e.g., ocean acidification). CDIAC has provided data management support for numerous long-term measurement projects crucial to climate change science. One current example is the AmeriFlux measurement network. AmeriFlux provides continuous measurements from forests, grasslands, wetlands, and croplands in North, Central, and South America and offers important insight about carbon cycling in terrestrial ecosystems. We share our approaches in satisfying the challenges of delivering AmeriFlux data worldwide to benefit others with similar challenges handling climate change data, further heighten awareness and use of an outstanding ecological data resource, and highlight expanded software engineering applications being used for climate change measurement data.

  13. Renewable Energy and Climate Change

    SciTech Connect (OSTI)

    Chum, H. L.

    2012-01-01T23:59:59.000Z

    The Intergovernmental Panel on Climate Change issued the Special Report on Renewable Energy Sources and Climate Change Mitigation (SRREN) at http://srren.ipcc-wg3.de/ (May 2011 electronic version; printed form ISBN 978-1-107-60710-1, 2012). More than 130 scientists contributed to the report.* The SRREN assessed existing literature on the future potential of renewable energy for the mitigation of climate change within a portfolio of mitigation options including energy conservation and efficiency, fossil fuel switching, RE, nuclear and carbon capture and storage (CCS). It covers the six most important renewable energy technologies - bioenergy, direct solar, geothermal, hydropower, ocean and wind, as well as their integration into present and future energy systems. It also takes into consideration the environmental and social consequences associated with these technologies, the cost and strategies to overcome technical as well as non-technical obstacles to their application and diffusion.

  14. Precipitation extremes under climate change

    E-Print Network [OSTI]

    O'Gorman, Paul A

    2015-01-01T23:59:59.000Z

    The response of precipitation extremes to climate change is considered using results from theory, modeling, and observations, with a focus on the physical factors that control the response. Observations and simulations with climate models show that precipitation extremes intensify in response to a warming climate. However, the sensitivity of precipitation extremes to warming remains uncertain when convection is important, and it may be higher in the tropics than the extratropics. Several physical contributions govern the response of precipitation extremes. The thermodynamic contribution is robust and well understood, but theoretical understanding of the microphysical and dynamical contributions is still being developed. Orographic precipitation extremes and snowfall extremes respond differently from other precipitation extremes and require particular attention. Outstanding research challenges include the influence of mesoscale convective organization, the dependence on the duration considered, and the need to...

  15. Compressor Selection and Equipment Sizing for Cold Climate Heat Pumps

    SciTech Connect (OSTI)

    Shen, Bo [ORNL] [ORNL; Abdelaziz, Omar [ORNL] [ORNL; Rice, C Keith [ORNL] [ORNL

    2014-01-01T23:59:59.000Z

    In order to limit heating capacity degradation at -25 C (-13 F) ambient to 25%, compared to the nominal rating point capacity at 8.3 C (47 F), an extensive array of design and sizing options were investigated, based on fundamental equipment system modeling and building energy simulation. Sixteen equipment design options were evaluated in one commercial building and one residential building, respectively in seven cities. The energy simulation results were compared to three baseline cases: 100% electric resistance heating, a 9.6 HSPF single-speed heat pump unit, and 90% AFUE gas heating system. The general recommendation is that variable-speed compressors and tandem compressors, sized such that their rated heating capacity at a low speed matching the building design cooling load, are able to achieve the capacity goal at low ambient temperatures by over-speeding, for example, a home with a 3.0 ton design cooling load, a tandem heat pump could meet this cooling load running a single compressor, while running both compressors to meet heating load at low ambient temperatures in a cold climate. Energy savings and electric resistance heat reductions vary with building types, energy codes and climate zones. Oversizing a heat pump can result in larger energy saving in a less energy efficient building and colder regions due to reducing electric resistance heating. However, in a more energy-efficient building or for buildings in warmer climates, one has to consider balance between reduction of resistance heat and addition of cyclic loss.

  16. Climate Action Plans and Long-Range Transportation

    E-Print Network [OSTI]

    Bertini, Robert L.

    Climate Action Plans and Long-Range Transportation Plans in the Pacific Northwest: A Review Climate Change and Impacts Mitigation versus Adaptation Impacts of Climate Change: Nation & the Pacific Northwest Climate Change Planning Efforts Transportation Sector Response - Survey Recommendations Continued

  17. Chaos, storms and climate on Mars

    E-Print Network [OSTI]

    Kite, Edwin S; Michaels, Timothy; Dietrich, William E; Manga, Michael

    2011-01-01T23:59:59.000Z

    Channel networks on the plateau adjacent to Juventae Chasma have the highest drainage densities reported on Mars.We model frozen precipitation on the Juventae plateau,finding that the trigger for forming these channel networks could have been ephemeral lakeshore precipitation,and that they do not require past temperatures higher than today.If short-lived and localized events explain some dendritic channel networks on Mars, this would weaken the link between dendritic valley networks and surface climate conditions that could sustain life. Our analysis uses MRAMS simulations and HiRISE DTMs.We model localized weather systems driven by water vapor release from ephemeral lakes during outflow channel formation.At Juventae Chasma,mean snowfall reaches a maximum of 0.9mm/hr water equivalent on the SW rim of the chasm.Radiative effects of the thick cloud cover raise maximum (minimum, mean) plateau surface temperatures by up to 24K(9K, 17K)locally.The key result is that the area of maximum modeled precipitation shows ...

  18. Climate Vulnerabilities | Department of Energy

    Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

    AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home Page onYouTube YouTube Note: Since the YouTube platformBuilding RemovalCSSDepartmentDepartmentBoston,ClimateClimate

  19. PUBLISHED ONLINE: 20 DECEMBER 2009 | DOI: 10.1038/NGEO724 High Earth-system climate sensitivity determined

    E-Print Network [OSTI]

    Cai, Long

    small rise in atmospheric CO2 levels was associated with substantial global warming about 4.5 million LaRiviere3 and Ana Christina Ravelo3 Climate sensitivity--the mean global temperature response years ago, and that CO2 levels at peak temperatures were between about 365 and 415 ppm. We conclude

  20. Projected impacts of climate change on species distribution in the Acadian Forest region of eastern Nova Scotia

    E-Print Network [OSTI]

    .e., hydrological cycle and earth- sun geometry. Growing degree days and mean air temperature are basedProjected impacts of climate change on species distribution in the Acadian Forest region of eastern on processing remote sensing data, mean air temperatures serves as one of several inputs to model calculation