Future Climate Change Under SSP Emission Scenarios With GISS‐E2.1
Authors: Nazarenko Larissa S. , Tausnev Nick , Russell Gary L. , Rind David , Miller Ron L. , Schmidt Gavin A. , Bauer Susanne E. , Kelley Maxwell , Ruedy Reto , Ackerman Andrew S. , Aleinov Igor , Bauer Michael , Bleck Rainer , Canuto Vittorio , Cesana Grégory , Cheng Ye , Clune Thomas L. , Cook Ben I. , Cruz Carlos A. , Del Genio Anthony D. , Elsaesser Gregory S. , Faluvegi Greg , Kiang Nancy Y. , Kim Daehyun , Lacis Andrew A. , Leboissetier Anthony , LeGrande Allegra N. , Lo Ken K. , Marshall John , Matthews Elaine E. , McDermid Sonali , Mezuman Keren , Murray Lee T. , Oinas Valdar , Orbe Clara , García‐Pando Carlos Pérez , Perlwitz Jan P. , Puma Michael J. , Romanou Anastasia , Shindell Drew T. , Sun Shan , Tsigaridis Kostas , Tselioudis George , Weng Ensheng , Wu Jingbo , Yao Mao‐Sung 
Published: March 2022

This paper presents the response to anthropogenic forcing in the GISS‐E2.1 climate models for the 21st century Shared Socioeconomic Pathways emission scenarios within the Coupled Model Intercomparison Project Phase 6 (CMIP6). The experiments were performed using an updated and improved version of the NASA Goddard Institute for Space Studies (GISS) coupled general circulation model that includes two different versions for atmospheric composition: A non‐interactive version (NINT) with prescribed composition and a tuned aerosol indirect effect and the One‐Moment Aerosol model (OMA) version with fully interactive aerosols which includes a parameterized first indirect aerosol effect on clouds. The effective climate sensitivities are 3.0°C and 2.9°C for the NINT and OMA models, respectively. Each atmospheric version is coupled to two different ocean general circulation models: The GISS ocean model (E2.1‐G) and HYCOM (E2.1‐H). We describe the global mean responses for all future scenarios and spatial patterns of change for surface air temperature and precipitation for four of the marker scenarios: SSP1‐2.6, SSP2‐4.5, SSP4‐6.0, and SSP5‐8.5. By 2100, global mean warming ranges from 1.5°C to 5.2°C relative to 1,850–1,880 mean temperature. Two high‐mitigation scenarios SSP1‐1.9 and SSP1‐2.6 limit the surface warming to below 2°C by the end of the 21st century, except for the NINT E2.1‐H model that simulates 2.2°C of surface warming. For the high emission scenario SSP5‐8.5, the range is 4.6–5.2°C at 2100. Due to about 15% larger effective climate sensitivity and stronger transient climate response in both NINT and OMA CMIP6 models compared to CMIP5 versions, there is a stronger warming by 2100 in the SSP emission scenarios than in the comparable Representative Concentration Pathway (RCP) scenarios in CMIP5. Changes in sea ice area are highly correlated to global mean surface air temperature anomalies and show steep declines in both hemispheres, with the largest sea ice area decreases occurring during September in the Northern Hemisphere in both E2.1‐G (−1.21 × 106 km2/°C) and E2.1‐H models (−0.94 × 106 km2/°C). Both coupled models project decreases in the Atlantic overturning stream function by 2100. The largest decrease of 56%–65% in the 21st century overturning stream function is produced in the warmest scenario SSP5‐8.5 in the E2.1‐G model, comparable to the reduction in the corresponding CMIP5 GISS‐E2 RCP8.5 simulation. Both low‐end scenarios SSP1‐1.9 and SSP1‐2.6 also simulate substantial reductions of the overturning (9%–37%) with slow recovery of about 10% by the end of the 21st century (relative to the maximum decrease at the middle of the 21st century).