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Future Antarctic Climate: Storylines of Midlatitude Jet Strengthening and Shift Emergent from CMIP6

Authors :
Williams, Ryan S.
Marshall, Gareth J.
Levine, Xavier
Graff, Lise S.
Handorf, Dörthe
Johnston, Nadine M.
Karpechko, Alexey Y.
Orr, Andrew
van de Berg, Willem Jan
Wijngaard, René R.
Mooney, Priscilla A.
Williams, Ryan S.
Marshall, Gareth J.
Levine, Xavier
Graff, Lise S.
Handorf, Dörthe
Johnston, Nadine M.
Karpechko, Alexey Y.
Orr, Andrew
van de Berg, Willem Jan
Wijngaard, René R.
Mooney, Priscilla A.
Source :
Journal of Climate vol.37 (2024) date: 2024-03-31 nr.7 p.2157-2178 [ISSN 0894-8755]
Publication Year :
2024

Abstract

A main source of regional climate change uncertainty is the large disparity across models in simulating the atmospheric circulation response to global warming. Using the latest suite of global climate models from the sixth phase of the Coupled Model Intercomparison Project (CMIP6), a storyline approach is adopted to derive physically plausible scenarios of Antarctic climate change for 2070–99, according to Shared Socioeconomic Pathway SSP5-8.5. These storylines correspond to differences in the simulated amount of seasonal sea ice loss and either (i) the delay in the summertime stratospheric polar vortex (SPV) breakdown or (ii) wintertime SPV strengthening, which together constitute robust drivers of the response pattern to future climate change. Such changes combined are known to exert a strong control over the Southern Hemisphere midlatitude jet stream, which we quantify as collectively explaining up to 70% of the variance in jet response in summer and 35% in winter. For summer, the expected strengthening and displacement of the tropospheric jet stream varies between a;1 and 2 m s21 increase and;28–48 poleward shift, respectively, across storylines. In both seasons, a larger strengthening of the jet is correlated with less Antarctic warming. By contrast, the response in precipitation is more consistent but still strongly attenuated by large-scale dynamics. We find that an increase in high-latitude precipitation around Antarctica is more pronounced for storylines characterized by a greater poleward jet shift, particularly in summer. Our results highlight the usefulness of the storyline approach in illustrating model uncertainty and understanding the processes that determine the spread in projected Antarctic regional climate response. SIGNIFICANCE STATEMENT: Uncertainty in future climate predictions for the Antarctic is dominated by the unknown response of the large-scale (global) atmospheric circulation. In characterizing such uncertainty, plausible ou

Details

Database :
OAIster
Journal :
Journal of Climate vol.37 (2024) date: 2024-03-31 nr.7 p.2157-2178 [ISSN 0894-8755]
Notes :
DOI: 10.1175/JCLI-D-23-0122.1, English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1445834637
Document Type :
Electronic Resource