Future climate change under RCP emission scenarios with GISS ModelE2

Nazarenko, L.; Schmidt, G. A.; Miller, R. L.; Tausnev, N.; Kelley, M.; Ruedy, R.; Russell, G. L.; Aleinov, I.; Bauer, M.; Bauer, S.; Bleck, R.; Canuto, V.; Cheng, Y.; Clune, T. L.; Del Genio, A. D.; Faluvegi, G.; Hansen, J. E.; Healy, R. J.; Kiang, N. Y.; Koch, D.; Lacis, A. A.; LeGrande, A. N.; Lerner, J.; Lo, K. K.; Menon, S.; Oinas, V.; Perlwitz, J.; Puma, M. J.; Rind, D.; Romanou, A.; Sato, M.; Shindell, D. T.; Sun, S.; Tsigaridis, K.; Unger, N.; Voulgarakis, A.; Yao, M. -S.; Zhang, Jinlun

doi:10.1002/2014MS000403

Title: Future climate change under RCP emission scenarios with GISS ModelE2

Journal Article · Tue Feb 24 00:00:00 EST 2015 · Journal of Advances in Modeling Earth Systems

DOI:https://doi.org/10.1002/2014MS000403· OSTI ID:1191174

Nazarenko, L. ^[1]; Schmidt, G. A. ^[2]; Miller, R. L. ^[2]; Tausnev, N. ^[3]; Kelley, M. ^[3]; Ruedy, R. ^[3]; Russell, G. L. ^[2]; Aleinov, I. ^[1]; Bauer, M. ^[4]; Bauer, S. ^[5]; Bleck, R. ^[6]; Canuto, V. ^[6]; Cheng, Y. ^[5]; Clune, T. L. ^[7]; Del Genio, A. D. ^[2]; Faluvegi, G. ^[5]; Hansen, J. E. ^[4]; Healy, R. J. ^[8]; Kiang, N. Y. ^[2]; Koch, D. ^[9] more »

Columbia Univ., New York, NY (United States); NASA Goddard Institute for Space Studies, New York, NY (United States)
NASA Goddard Inst. for Space Studies (GISS), New York, NY (United States)
NASA Goddard Inst. for Space Studies (GISS), New York, NY (United States); Trinnovim LLC, New York, NY (United States)
NASA Goddard Inst. for Space Studies (GISS), New York, NY (United States); Columbia Univ., New York, NY (United States)
Columbia Univ., New York, NY (United States); NASA Goddard Inst. for Space Studies (GISS), New York, NY (United States)
Columbia Univ., New York, NY (United States)
NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States)
Columbia Univ., New York, NY (United States); NASA Goddard Inst. for Space Studies (GISS), New York, NY (United States);
Columbia Univ., New York, NY (United States); USDOE, Washington, DC (United States)
Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
Yale Univ., New Haven, CT (United States)
Columbia Univ., New York, NY (United States); Trinnovim LLC, New York, NY (United States)
Univ. of Washington, Seattle, WA (United States)

We examine the anthropogenically forced climate response for the 21st century representative concentration pathway (RCP) emission scenarios and their extensions for the period 2101–2500. The experiments were performed with ModelE2, a new version of the NASA Goddard Institute for Space Sciences (GISS) coupled general circulation model that includes three different versions for the atmospheric composition components: a noninteractive version (NINT) with prescribed composition and a tuned aerosol indirect effect (AIE), the TCAD version with fully interactive aerosols, whole-atmosphere chemistry, and the tuned AIE, and the TCADI version which further includes a parameterized first indirect aerosol effect on clouds. Each atmospheric version is coupled to two different ocean general circulation models: the Russell ocean model (GISS-E2-R) and HYCOM (GISS-E2-H). By 2100, global mean warming in the RCP scenarios ranges from 1.0 to 4.5° C relative to 1850–1860 mean temperature in the historical simulations. In the RCP2.6 scenario, the surface warming in all simulations stays below a 2 °C threshold at the end of the 21st century. For RCP8.5, the range is 3.5–4.5° C at 2100. Decadally averaged sea ice area changes are highly correlated to global mean surface air temperature anomalies and show steep declines in both hemispheres, with a larger sensitivity during winter months. By the year 2500, there are complete recoveries of the globally averaged surface air temperature for all versions of the GISS climate model in the low-forcing scenario RCP2.6. TCADI simulations show enhanced warming due to greater sensitivity to CO₂, aerosol effects, and greater methane feedbacks, and recovery is much slower in RCP2.6 than with the NINT and TCAD versions. All coupled models have decreases in the Atlantic overturning stream function by 2100. In RCP2.6, there is a complete recovery of the Atlantic overturning stream function by the year 2500 while with scenario RCP8.5, the E2-R climate model produces a complete shutdown of deep water formation in the North Atlantic.

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Research Organization:: Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)

Sponsoring Organization:: USDOE; National Aeronautics and Space Administration (NASA)

Grant/Contract Number:: AC02-05CH11231

OSTI ID:: 1191174

Journal Information:: Journal of Advances in Modeling Earth Systems, Vol. 7, Issue 1; ISSN 1942-2466

Publisher:: American Geophysical Union (AGU)Copyright Statement

Country of Publication:: United States

Language:: English

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Cited by: 90 works

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Change of niche in guanaco (Lama guanicoe): The effects of climate change on habitat suitability and lineage conservatism in Chile Castillo, Andrea G.; Alò, Dominique; González, Benito A. PeerJ Preprints https://doi.org/10.7287/peerj.preprints.3517v1	posted_content	January 2018
On the relationship between GHGs and Global Temperature Anomalies: Multi-level rolling analysis and Copula calibration Agliardi, Elettra; Alexopoulos, Thomas; Cech, Christian Unpublished https://doi.org/10.13140/rg.2.2.32216.08969	text	January 2017
Range-wide variation in local adaptation and phenotypic plasticity of fitness-related traits in Fagus sylvatica and their implications under climate change Gárate-Escamilla, Homero; Hampe, Arndt; Vizcaíno-Palomar, Natalia bioRxiv https://doi.org/10.1101/513515	posted_content	January 2019
Tropical cyclones in the GISS ModelE2 Camargo, Suzana J.; Sobel, Adam H.; Del Genio, Anthony D. Columbia University https://doi.org/10.7916/d8-2ymh-8911	text	January 2016

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