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GISS-E2.1: Configurations and Climatology.

Maxwell KelleyGavin A SchmidtLarissa S NazarenkoSusanne E BauerReto RuedyGary L RussellAndrew S AckermanIgor AleinovMichael BauerRainer BleckVittorio CanutoGrégory CesanaYe ChengThomas L CluneBen I CookCarlos A CruzAnthony D Del GenioGregory S ElsaesserGregory FaluvegiNancy Y KiangDaehyun KimAndrew A LacisAnthony LeboissetierAllegra N LeGrandeKen K LoJohn MarshallElaine E MatthewsSonali Shukla McDermidKeren MezumanRon L MillerLee T MurrayValdar OinasClara OrbeCarlos Pérez García-PandoJan P PerlwitzMichael J PumaDavid RindAnastasia RomanouDrew T ShindellShan SunNick TausnevKostas TsigaridisGeorge TselioudisEnsheng WengJingbo WuMao-Sung Yao
Published in: Journal of advances in modeling earth systems (2020)
This paper describes the GISS-E2.1 contribution to the Coupled Model Intercomparison Project, Phase 6 (CMIP6). This model version differs from the predecessor model (GISS-E2) chiefly due to parameterization improvements to the atmospheric and ocean model components, while keeping atmospheric resolution the same. Model skill when compared to modern era climatologies is significantly higher than in previous versions. Additionally, updates in forcings have a material impact on the results. In particular, there have been specific improvements in representations of modes of variability (such as the Madden-Julian Oscillation and other modes in the Pacific) and significant improvements in the simulation of the climate of the Southern Oceans, including sea ice. The effective climate sensitivity to 2 × CO2 is slightly higher than previously at 2.7-3.1°C (depending on version) and is a result of lower CO2 radiative forcing and stronger positive feedbacks.
Keyphrases
  • climate change
  • high frequency