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CMIP5 model selection for ISMIP6 ice sheet model forcing: Greenland and Antarctica

Authors :
Christopher M. Little
Cécile Agosta
Heiko Goelzer
Sophie Nowicki
Helene Seroussi
Thomas J. Bracegirdle
Fiammetta Straneo
Nicolas C. Jourdain
Tore Hattermann
Alice Barthel
Los Alamos National Laboratory (LANL)
Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Glaces et Continents, Climats et Isotopes Stables (GLACCIOS)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Atmospheric and Environmental Research, Inc. (AER)
Norwegian Polar Institute
Institut des Géosciences de l’Environnement (IGE)
Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )
Université Grenoble Alpes (UGA)
Institute for Marine and Atmospheric Research [Utrecht] (IMAU)
Utrecht University [Utrecht]
NASA Goddard Space Flight Center (GSFC)
Jet Propulsion Laboratory (JPL)
NASA-California Institute of Technology (CALTECH)
Scripps Institution of Oceanography (SIO)
University of California [San Diego] (UC San Diego)
University of California-University of California
British Antarctic Survey (BAS)
Natural Environment Research Council (NERC)
ANR-15-CE01-0015,AC-AHC2,Circulation atmosphérique et changement de cycle hydrologique pour l'Arctique(2015)
ANR-15-CE01-0005,TROIS-AS,Vers un système de modélisation régionale océan / calotte / atmosphère(2015)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)
Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )
Scripps Institution of Oceanography (SIO - UC San Diego)
University of California (UC)-University of California (UC)
Sub Dynamics Meteorology
Marine and Atmospheric Research
Source :
The Cryosphere, The Cryosphere, Copernicus 2020, 14 (3), pp.855-879. ⟨10.5194/tc-14-855-2020⟩, The Cryosphere, 2020, 14 (3), pp.855-879. ⟨10.5194/tc-14-855-2020⟩, Cryosphere, 14(3), 855. Copernicus Publications, The Cryosphere, 14 (3, The Cryosphere, Vol 14, Pp 855-879 (2020)
Publication Year :
2020
Publisher :
HAL CCSD, 2020.

Abstract

The ice sheet model intercomparison project for CMIP6 (ISMIP6) effort brings together the ice sheet and climate modeling communities to gain understanding of the ice sheet contribution to sea level rise. ISMIP6 conducts stand-alone ice sheet experiments that use space- and time-varying forcing derived from atmosphere-ocean coupled global climate models (AOGCMs) to reflect plausible trajectories for climate projections. The goal of this study is to recommend a subset of CMIP5 AOGCMs (three core and three targeted) to produce forcing for ISMIP6 stand-alone ice sheet simulations, based on (i) their representation of current climate near Antarctica and Greenland relative to observations and (ii) their ability to sample a diversity of projected atmosphere and ocean changes over the 21st century. The selection is performed separately for Greenland and Antarctica. Model evaluation over the historical period focuses on variables used to generate ice sheet forcing. For stage (i), we combine metrics of atmosphere and surface ocean state (annual- and seasonal-mean variables over large spatial domains) with metrics of time-mean subsurface ocean temperature biases averaged over sectors of the continental shelf. For stage (ii), we maximize the diversity of climate projections among the best-performing models. Model selection is also constrained by technical limitations, such as availability of required data from RCP2.6 and RCP8.5 projections. The selected top three CMIP5 climate models are CCSM4, MIROC-ESM-CHEM, and NorESM1-M for Antarctica and HadGEM2-ES, MIROC5, and NorESM1-M for Greenland. This model selection was designed specifically for ISMIP6 but can be adapted for other applications.<br />SCOPUS: ar.j<br />info:eu-repo/semantics/published

Details

Language :
English
ISSN :
19940424 and 19940416
Database :
OpenAIRE
Journal :
The Cryosphere, The Cryosphere, Copernicus 2020, 14 (3), pp.855-879. ⟨10.5194/tc-14-855-2020⟩, The Cryosphere, 2020, 14 (3), pp.855-879. ⟨10.5194/tc-14-855-2020⟩, Cryosphere, 14(3), 855. Copernicus Publications, The Cryosphere, 14 (3, The Cryosphere, Vol 14, Pp 855-879 (2020)
Accession number :
edsair.doi.dedup.....a701502689b300753e4f6102d37631bc
Full Text :
https://doi.org/10.5194/tc-14-855-2020⟩