
- Large discrepancy between observed and simulated precipitation trends in the ascending and descending branches of the tropical
- Spinning column of air Associated with strong updraught and
- Water vapor variability in the tropics and its links to dynamics and precipitation
- Inconsistencies between satellite estimates of longwave cloud forcing and dynamical fields from reanalyses
- Current changes in tropical precipitation This article has been downloaded from IOPscience. Please scroll down to see the full text article.
- Evaluation of the model representation of the evolution of convective systems using satellite observations of outgoing
- metal. This is caused by strong interactions between the meta-atoms.
- Diagnostic analysis of atmospheric moisture and clear-sky radiative feedback in the Hadley
- down on greater slopes, the deposits could eventually become even steeper because the
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 133: 19932010 (2007)
- THE GEOSTATIONARY EARTH RADIATION BUDGET PROJECT
- monthly averages also results from the natural vari-ability when few measurements are available.
- A case study of the radiative forcing of persistent contrails evolving into contrail-induced cirrus
- Exploitation of Geostationary Earth Radiation Budget data using simulations from a numerical
- JOURNAL OF GEOPHYSICAL RESEARCH, VOL. ???, XXXX, DOI:10.1029/, Clear-sky biases in satellite infrared estimates of1
- Royal Meteorological Society 2 www.noaa.gov
- Red sky at night: There are various explanations but the key is the fact that the sun rises in the East and weather tends to move in from
- Q. J. R. Meteorol. Soc. (2003), 129, pp. 33713389 doi: 10.1256/qj.02.217 Evaluation of moisture in the Hadley Centre climate model using
- Royal Meteorological Society WEATHER SYSTEMS
- Current changes in tropical precipitation Richard P. Allan1
- INTERNATIONAL JOURNAL OF CLIMATOLOGY Int. J. Climatol. (2010)
- SINERGEE: SIMULATION AND EXPLOITATION OF DATA FROM METEOSAT-8 USING AN NWP MODEL
- Clouds are integral to the climate system. They are a crucial component of the global water cycle,
- Changes in Tropical Clouds and Two potentially important papers by
- www.sciencemag.org SCIENCE VOL 295 1 FEBRUARY 2002 811 the horizontal momentum direction by pB.
- INVESTIGATION OF TRENDS IN THE MOISTURE BUDGET OF THE TROPICAL
- University of Reading Department of Meteorology
- MRF Technical Note # 49 Can desert dust explain the anomalous greenhouse
- Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. (2010) Examination of long-wave radiative bias in general circulation
- Summertime precipitation variability over Europe and its links to atmospheric dynamics and evaporation
- 9.12 EVALUATION OF CLIMATE-MODEL SIMULATIONS OF HIRS WATER-VAPOUR CHANNEL RADIANCES
- Royal Meteorological Society 1 INTRODUCTION TO CLOUDS
- Summertime Precipitation Variability over Europe and its1 Links to Atmospheric Dynamics and Evaporation2
- Differences in the evolution of seismic velocities after the San Simeon and the Parkfield earthquakes
- Simulation of the Earth's radiation budget by the European Centre for Medium-Range Weather
- USING SATELLITE OBSERVATIONS AND REANALYSES TO EVALUATE CLIMATE AND WEATHER FORECAST MODELS
- REVIEW ARTICLE How Well Do We Understand and Evaluate Climate Change Feedback Processes?
- Anticipated changes in the global atmospheric water cycle This article has been downloaded from IOPscience. Please scroll down to see the full text article.
- Temperature (T) degrees Celsius (oC) arbitrary scale from 0oC at melting point of ice to 100oC at
- Observations of the diurnal cycle of outgoing longwave radiation from the Geostationary Earth Radiation Budget instrument
- Energy Budgets: From a Person to a Planet
- INTERNATIONAL JOURNAL OF CLIMATOLOGY Int. J. Climatol. 31: 337348 (2011)
- How robust are observed and simulated precipitation responses to tropical ocean warming?
- Overview of observations from the RADAGAST experiment in Niamey, Niger: Meteorology and thermodynamic variables
- Observations of the impact of a major Saharan dust storm on the atmospheric radiation balance
- Variability in clear-sky longwave radiative cooling of the atmosphere
- Can desert dust explain the outgoing longwave radiation anomaly over the Sahara during July 2003?
- Tellus (2004), 56A, 308327 Copyright C Blackwell Munksgaard, 2004 Printed in UK. All rights reserved TELLUS
- Q. J. R. Meteorol. Soc. (2003), 129, pp. 29712988 doi: 10.1256/qj.02.216 Simulations of the effects of interannual and decadal variability on the clear-sky
- Investigating the Radiative Impact Clouds Using Retrieved Properties to Classify Cloud Type
- IPCC Workshop on Climate Sensitivity Paris, France, July 2629, 2004
- STRATEGIES FOR DETERMINING CLEAR SKY FLUXES FROM GERB J E Russell1
- THE GEOSTATIONARY EARTH RADIATION BUDGET (GERB) EXPERIMENT: SCIENCE AND APPLICATIONS
- Using ERA-40 products to verify and improve the Met Office climate model
- Figure 1: Mean 500 hPa vertical velocity (hPa day-1 ) from (a) ERA, (b) HadAM3
- www.sciencemag.org/cgi/content/full/1160787/DC1 Supporting Online Material for
- Tellus (2007), 59A, 336343 C 2007 The Author Journal compilation C 2007 Blackwell Munksgaard
- Q U A R T E R L Y J O U R N A L R O Y A L M E T E O R O L O G I C A L S O C I E T Y
- 3080 VOLUME 13J O U R N A L O F C L I M A T E Water Vapor Feedbacks in the ECMWF Reanalyses and Hadley Centre Climate Model
- Update this !!! What measures climate? A variety of variables including their variability and
- Climate changes on all time-scales. One of the most important determinants of climate is variations in the
- Tellus (2008), 60A, 3241 C 2007 The Authors Journal compilation C 2007 Blackwell Munksgaard
- 15 JULY 2002 1979A L L A N E T A L . Influence of Dynamics on the Changes in Tropical Cloud Radiative Forcing
- 1 JUNE 2000 1951A L L A N Evaluation of Simulated Clear-Sky Longwave Radiation Using
- Simulated Longwave Clearsky Irradiance over the Ocean: Spatial and Temporal Variability 19791993
- Online at www.sciencemag.org/cgi/content/full/295/ 5556/838/DC1.
- Examination of Relationships between Clear-Sky Longwave Radiation and Aspects of the Atmospheric Hydrological Cycle in Climate Models, Reanalyses, and Observations
- Analysis of moisture variability in the European Centre for Medium-Range Weather Forecasts 15-year
- MONITORING PRESENT DAY CHANGES IN WATER VAPOUR AND THE RADIATIVE ENERGY BALANCE USING SATELLITE DATA,
- Regime dependent changes in global precipitation Richard P. Allan
- Clearsky biases in satellite infrared estimates of upper tropospheric humidity and its trends
- METEOROLOGICAL APPLICATIONS Meteorol. Appl. 18: 324333 (2011)
- Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. 137: 11061116, July 2011 A Motivation, rationale and key results from the GERBILS
- Surveys in Geophysics manuscript No. (will be inserted by the editor)
- Multi-satellite observed responses of precipitation and its extremes to3 interannual climate variability4
- Richard P. Allan: Curriculum Vitae r.p.allan@reading.ac.uk +44 (0)118 3785568
- Surveys in Geophysics The role of water vapour in Earth's energy flows
- Phys. Chem. Earth, Vol. 23, No. 5-6, pp. 599-604, 1998 1998 Elsevier Scienc~ Ltd.
- University of Reading Department of Meteorology
- Richard P. Allan: Curriculum Vitae r.p.allan@reading.ac.uk +44 (0)118 3785568
- JOHN WILEY & SONS, LTD., THE ATRIUM, SOUTHERN GATE, CHICHESTER P019 8SQ, UK ***PROOF OF YOUR ARTICLE ATTACHED, PLEASE READ CAREFULLY***
- Winter floods in Britain are connected to atmospheric rivers David A. Lavers,1,2
- Q. J. R. Mereorul. Soc. (1999). 125, pp. 2103-2126 The dependence of clear-sky outgoing long-wave radiation on surface
- Observing Changes in Earth's Energy Budget During the Past Decade Norman G. Loeb1*
- Changes in water vapor transports of the ascending branch of the tropical circulation
- METEOROLOGICAL APPLICATIONS Meteorol. Appl. (2012)
- Multisatellite observed responses of precipitation and its extremes to interannual climate variability
- PUBLISHED ONLINE: 22 JANUARY 2012 | DOI: 10.1038/NGEO1375 Observed changes in top-of-the-atmosphere