DC Field | Value | Language |
---|---|---|
dc.contributor.author | Lim, H.-G | - |
dc.contributor.author | Yeh, S.-W | - |
dc.contributor.author | Kug, Jong-Seong | - |
dc.contributor.author | Park, Y.-G | - |
dc.contributor.author | Park, J.-H | - |
dc.contributor.author | Park, R | - |
dc.contributor.author | Song, C.-K. | - |
dc.date.accessioned | 2017-07-19T13:32:16Z | - |
dc.date.available | 2017-07-19T13:32:16Z | - |
dc.date.created | 2017-02-15 | - |
dc.date.issued | 2016-06 | - |
dc.identifier.issn | 0930-7575 | - |
dc.identifier.uri | https://oasis.postech.ac.kr/handle/2014.oak/37183 | - |
dc.description.abstract | In order to examine the threshold of the volcanic forcing that leads to the El Nino-like warming, we analyze a millennium ERIK simulation (AD 1000-1850) forced by three external forcings including greenhouse gases, solar forcing and volcanic eruptions using the ECHO-G coupled climate model. It is found that there exists a threshold of the volcanic forcing above 15 W/m(2) to lead the El Nino-like warming in the climate model. When the volcanic forcing is above this threshold forcing, then the intensity of the Inter-tropical Convergence Zone (ITCZ) is weakened and its position is shifted to the south. This might be associated with the processes of less evaporation in the subtropical cloudless region by a cooling due to the reduction of net surface shortwave radiation. Concurrently, a weakening of ITCZ is associated with a weakening of the trade winds and the subsequent Bjerknes feedback causes El Nino-like warming. Therefore, El Nino-like warming events can occur when volcanic eruption is above threshold forcing, implying that there exists a certain level of radiative forcing change which is capable of changing the state of tropical Pacific sea surface temperature. The last millennium simulation of Paleoclimate Modeling Intercomparison Project Phase 3 climate models also indicates that there may exist a threshold forcing to lead the El Nino-like warming, which has been also discussed in the present study. | - |
dc.language | English | - |
dc.publisher | CLIMATE DYNAMICS | - |
dc.relation.isPartOf | CLIMATE DYNAMICS | - |
dc.title | Threshold of the volcanic forcing that leads the El Nino-like warming in the last millennium: results from the ERIK simulation | - |
dc.type | Article | - |
dc.identifier.doi | 10.1007/S00382-015-2799-3 | - |
dc.type.rims | ART | - |
dc.identifier.bibliographicCitation | CLIMATE DYNAMICS, v.46, no.11-12, pp.3725 - 3736 | - |
dc.identifier.wosid | 000381108600021 | - |
dc.date.tcdate | 2019-02-01 | - |
dc.citation.endPage | 3736 | - |
dc.citation.number | 11-12 | - |
dc.citation.startPage | 3725 | - |
dc.citation.title | CLIMATE DYNAMICS | - |
dc.citation.volume | 46 | - |
dc.contributor.affiliatedAuthor | Kug, Jong-Seong | - |
dc.identifier.scopusid | 2-s2.0-84941335617 | - |
dc.description.journalClass | 1 | - |
dc.description.journalClass | 1 | - |
dc.description.wostc | 8 | - |
dc.type.docType | Article | - |
dc.subject.keywordPlus | 1000-YR CONTROL SIMULATION | - |
dc.subject.keywordPlus | ECHO-G | - |
dc.subject.keywordPlus | TROPICAL PACIFIC | - |
dc.subject.keywordPlus | ENSO | - |
dc.subject.keywordPlus | CLIMATE | - |
dc.subject.keywordPlus | SOLAR | - |
dc.subject.keywordPlus | VARIABILITY | - |
dc.subject.keywordPlus | TELECONNECTIONS | - |
dc.subject.keywordPlus | MODEL | - |
dc.subject.keywordPlus | AIR | - |
dc.relation.journalWebOfScienceCategory | Meteorology & Atmospheric Sciences | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.relation.journalResearchArea | Meteorology & Atmospheric Sciences | - |
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