A possible mechanism for El Nino-like warming in response to the future greenhouse warming SCIE SCOPUS
DC Field | Value | Language |
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dc.contributor.author | Kug, Jong-Seong | - |
dc.contributor.author | Sooraj, K. P. | - |
dc.contributor.author | Jin, Fei-Fei | - |
dc.contributor.author | Ham, Yoo-Geun | - |
dc.contributor.author | Kim, Daehyun | - |
dc.date.accessioned | 2020-04-20T07:43:35Z | - |
dc.date.available | 2020-04-20T07:43:35Z | - |
dc.date.created | 2020-01-28 | - |
dc.date.issued | 2011-08 | - |
dc.identifier.issn | 0899-8418 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/3833 | - |
dc.description.abstract | Using the climate change experiments generated for the Fourth Assessment of the Intergovernmental Panel on Climate Change, a possible mechanism for the El Nino-like warming in response to the greenhouse warming is suggested. From the coupled global climate model (CGCM) simulations with climate change scenario, it is found that the Bjerknes air-sea coupled process is a dominant contributor to the tropical Pacific response. However, it is revealed that most CGCMs commonly simulate the off-equatorial maximum of precipitation change. It is suggested here that the off-equatorial precipitation and the associated equatorial westerlies play a seeding role in triggering an El Nino-like warming response. Atmospheric GCM (AGCM) experiments show that even uniform sea-surface temperature (SST) warming leads to off-equatorial increase in precipitation which brings equatorial westerlies, implying that these non-uniform (off-equatorial) responses can play a seeding role for the El Nino-like warming pattern. Copyright (C) 2010 Royal Meteorological Society | - |
dc.description.uri | 1 | - |
dc.language | English | - |
dc.publisher | WILEY-BLACKWELL | - |
dc.subject | TROPICAL PACIFIC | - |
dc.subject | CLIMATE SENSITIVITY | - |
dc.subject | EQUATORIAL PACIFIC | - |
dc.subject | INCREASED CO2 | - |
dc.subject | OCEAN | - |
dc.subject | TERMINATION | - |
dc.subject | MODEL | - |
dc.subject | EQUILIBRIUM | - |
dc.subject | TRENDS | - |
dc.subject | ENSO | - |
dc.title | A possible mechanism for El Nino-like warming in response to the future greenhouse warming | - |
dc.type | Article | - |
dc.citation.endPage | 1572 | - |
dc.citation.startPage | 1567 | - |
dc.citation.title | INTERNATIONAL JOURNAL OF CLIMATOLOGY | - |
dc.citation.volume | 31 | - |
dc.citation.number | 10 | - |
dc.contributor.alternativeName | 국종성 | - |
dc.identifier.bibliographicCitation | INTERNATIONAL JOURNAL OF CLIMATOLOGY, v.31, no.10, pp.1567 - 1572 | - |
dc.identifier.doi | 10.1002/joc.2163 | - |
dc.identifier.scopusid | 2-s2.0-79955035968 | - |
dc.identifier.wosid | 000293247600013 | - |
dc.type.docType | Article | - |
dc.description.journalClass | 1 | - |
dc.subject.keywordPlus | ENSO | - |
dc.subject.keywordPlus | TROPICAL PACIFIC | - |
dc.subject.keywordPlus | CLIMATE SENSITIVITY | - |
dc.subject.keywordPlus | EQUATORIAL PACIFIC | - |
dc.subject.keywordPlus | INCREASED CO2 | - |
dc.subject.keywordPlus | OCEAN | - |
dc.subject.keywordPlus | TERMINATION | - |
dc.subject.keywordPlus | MODEL | - |
dc.subject.keywordPlus | EQUILIBRIUM | - |
dc.subject.keywordPlus | TRENDS | - |
dc.subject.keywordAuthor | El Nino-like warming | - |
dc.subject.keywordAuthor | global warming | - |
dc.subject.keywordAuthor | climate change | - |
dc.relation.journalWebOfScienceCategory | Meteorology & Atmospheric Sciences | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.relation.journalResearchArea | Meteorology & Atmospheric Sciences | - |