Southern Ocean Control of 2°C Global Warming in Climate Models
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Shin, So-Jung | - |
dc.contributor.author | Yeh, Sang-Wook | - |
dc.contributor.author | An, Soon-Il | - |
dc.contributor.author | Keenlyside, Noel | - |
dc.contributor.author | Xie, Shang-Ping | - |
dc.contributor.author | Park, Jae-Heung | - |
dc.date.accessioned | 2023-07-24T10:07:37Z | - |
dc.date.available | 2023-07-24T10:07:37Z | - |
dc.date.created | 2023-03-13 | - |
dc.date.issued | 2023-01 | - |
dc.identifier.issn | 2328-4277 | - |
dc.identifier.uri | https://scholarworks.bwise.kr/hanyang/handle/2021.sw.hanyang/187606 | - |
dc.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. © 2022 The Authors. Earth's Future published by Wiley Periodicals LLC on behalf of American Geophysical Union. | - |
dc.language | 영어 | - |
dc.language.iso | en | - |
dc.publisher | John Wiley and Sons Inc | - |
dc.title | Southern Ocean Control of 2°C Global Warming in Climate Models | - |
dc.type | Article | - |
dc.contributor.affiliatedAuthor | Yeh, Sang-Wook | - |
dc.identifier.doi | 10.1029/2022EF003212 | - |
dc.identifier.scopusid | 2-s2.0-85147146795 | - |
dc.identifier.wosid | 000998896900001 | - |
dc.identifier.bibliographicCitation | Earth's Future, v.11, no.1, pp.1 - 15 | - |
dc.relation.isPartOf | Earth's Future | - |
dc.citation.title | Earth's Future | - |
dc.citation.volume | 11 | - |
dc.citation.number | 1 | - |
dc.citation.startPage | 1 | - |
dc.citation.endPage | 15 | - |
dc.type.rims | ART | - |
dc.type.docType | Article | - |
dc.description.journalClass | 1 | - |
dc.description.isOpenAccess | Y | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.relation.journalResearchArea | Environmental Sciences & Ecology | - |
dc.relation.journalResearchArea | Geology | - |
dc.relation.journalResearchArea | Meteorology & Atmospheric Sciences | - |
dc.relation.journalWebOfScienceCategory | Environmental Sciences | - |
dc.relation.journalWebOfScienceCategory | Geosciences, Multidisciplinary | - |
dc.relation.journalWebOfScienceCategory | Meteorology & Atmospheric Sciences | - |
dc.subject.keywordPlus | TOP-OF-ATMOSPHERE | - |
dc.subject.keywordPlus | HEAT UPTAKE | - |
dc.subject.keywordPlus | SEA-ICE | - |
dc.subject.keywordPlus | SENSITIVITY | - |
dc.subject.keywordPlus | CMIP5 | - |
dc.subject.keywordPlus | 1.5-DEGREES-C | - |
dc.subject.keywordPlus | TEMPERATURES | - |
dc.subject.keywordPlus | CIRCULATION | - |
dc.subject.keywordPlus | CONVECTION | - |
dc.subject.keywordPlus | CLOUDS | - |
dc.subject.keywordAuthor | Antarctic sea ice | - |
dc.subject.keywordAuthor | low level cloud amount feedback | - |
dc.subject.keywordAuthor | Paris agreement | - |
dc.subject.keywordAuthor | southern ocean condition | - |
dc.identifier.url | https://www.proquest.com/docview/2770083313?accountid=11283 | - |
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