Southern Ocean Control of 2°C Global Warming in Climate Models
Abstract Global warming will soon reach the Paris Agreement targets of 1.5°C/2°C temperature increase above pre‐industrial levels. Under a business‐as‐usual scenario, the time to reach these targets varies widely among climate models. Using Coupled Model Intercomparison Project Phase 5 and 6, we sho...
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ftdoajarticles:oai:doaj.org/article:f128ed3ff5344d1d911aea7400f06126 2023-05-15T13:31:44+02:00 Southern Ocean Control of 2°C Global Warming in Climate Models So‐Jung Shin Sang‐Wook Yeh Soon‐Il An Noel Keenlyside Shang‐Ping Xie Jae‐Heung Park 2023-01-01T00:00:00Z https://doi.org/10.1029/2022EF003212 https://doaj.org/article/f128ed3ff5344d1d911aea7400f06126 EN eng Wiley https://doi.org/10.1029/2022EF003212 https://doaj.org/toc/2328-4277 2328-4277 doi:10.1029/2022EF003212 https://doaj.org/article/f128ed3ff5344d1d911aea7400f06126 Earth's Future, Vol 11, Iss 1, Pp n/a-n/a (2023) southern ocean condition low level cloud amount feedback Paris agreement Antarctic sea ice Environmental sciences GE1-350 Ecology QH540-549.5 article 2023 ftdoajarticles https://doi.org/10.1029/2022EF003212 2023-01-29T01:26:13Z Abstract Global warming will soon reach the Paris Agreement targets of 1.5°C/2°C temperature increase above pre‐industrial levels. Under a business‐as‐usual scenario, the time to reach these targets varies widely among climate models. Using Coupled Model Intercomparison Project Phase 5 and 6, we show that a 2°C global warming is determined by Southern Ocean (SO) state closely tied with a low‐level cloud (LLC) amount feedback strength during reference (1861–1900) period; climate models with cold SO tend to accompany more low‐level cloudiness and Antarctic sea ice concentration due to a strong LLC amount feedback. Consequently, initially cold SO models tend to simulate a fast global warming by absorbing more downward shortwave radiation compared to initially warm SO models because more LLC disappears due to a strong LLC amount feedback during the 2°C rise. Our results demonstrate that climate models that correctly simulate initial SO state can improve 2°C warming projections with reduced uncertainties. Article in Journal/Newspaper Antarc* Antarctic Sea ice Southern Ocean Directory of Open Access Journals: DOAJ Articles Antarctic Southern Ocean Earth's Future 11 1 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
southern ocean condition low level cloud amount feedback Paris agreement Antarctic sea ice Environmental sciences GE1-350 Ecology QH540-549.5 |
spellingShingle |
southern ocean condition low level cloud amount feedback Paris agreement Antarctic sea ice Environmental sciences GE1-350 Ecology QH540-549.5 So‐Jung Shin Sang‐Wook Yeh Soon‐Il An Noel Keenlyside Shang‐Ping Xie Jae‐Heung Park Southern Ocean Control of 2°C Global Warming in Climate Models |
topic_facet |
southern ocean condition low level cloud amount feedback Paris agreement Antarctic sea ice Environmental sciences GE1-350 Ecology QH540-549.5 |
description |
Abstract Global warming will soon reach the Paris Agreement targets of 1.5°C/2°C temperature increase above pre‐industrial levels. Under a business‐as‐usual scenario, the time to reach these targets varies widely among climate models. Using Coupled Model Intercomparison Project Phase 5 and 6, we show that a 2°C global warming is determined by Southern Ocean (SO) state closely tied with a low‐level cloud (LLC) amount feedback strength during reference (1861–1900) period; climate models with cold SO tend to accompany more low‐level cloudiness and Antarctic sea ice concentration due to a strong LLC amount feedback. Consequently, initially cold SO models tend to simulate a fast global warming by absorbing more downward shortwave radiation compared to initially warm SO models because more LLC disappears due to a strong LLC amount feedback during the 2°C rise. Our results demonstrate that climate models that correctly simulate initial SO state can improve 2°C warming projections with reduced uncertainties. |
format |
Article in Journal/Newspaper |
author |
So‐Jung Shin Sang‐Wook Yeh Soon‐Il An Noel Keenlyside Shang‐Ping Xie Jae‐Heung Park |
author_facet |
So‐Jung Shin Sang‐Wook Yeh Soon‐Il An Noel Keenlyside Shang‐Ping Xie Jae‐Heung Park |
author_sort |
So‐Jung Shin |
title |
Southern Ocean Control of 2°C Global Warming in Climate Models |
title_short |
Southern Ocean Control of 2°C Global Warming in Climate Models |
title_full |
Southern Ocean Control of 2°C Global Warming in Climate Models |
title_fullStr |
Southern Ocean Control of 2°C Global Warming in Climate Models |
title_full_unstemmed |
Southern Ocean Control of 2°C Global Warming in Climate Models |
title_sort |
southern ocean control of 2°c global warming in climate models |
publisher |
Wiley |
publishDate |
2023 |
url |
https://doi.org/10.1029/2022EF003212 https://doaj.org/article/f128ed3ff5344d1d911aea7400f06126 |
geographic |
Antarctic Southern Ocean |
geographic_facet |
Antarctic Southern Ocean |
genre |
Antarc* Antarctic Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic Sea ice Southern Ocean |
op_source |
Earth's Future, Vol 11, Iss 1, Pp n/a-n/a (2023) |
op_relation |
https://doi.org/10.1029/2022EF003212 https://doaj.org/toc/2328-4277 2328-4277 doi:10.1029/2022EF003212 https://doaj.org/article/f128ed3ff5344d1d911aea7400f06126 |
op_doi |
https://doi.org/10.1029/2022EF003212 |
container_title |
Earth's Future |
container_volume |
11 |
container_issue |
1 |
_version_ |
1766020653249462272 |