Covariability of western tropical Pacific-North Pacific atmospheric circulation during summer
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Yun, Kyung-Sook | - |
dc.contributor.author | Yeh, Sang-Wook | - |
dc.contributor.author | Ha, Kyung-Ja | - |
dc.date.accessioned | 2021-06-22T18:42:57Z | - |
dc.date.available | 2021-06-22T18:42:57Z | - |
dc.date.created | 2021-01-21 | - |
dc.date.issued | 2015-11 | - |
dc.identifier.issn | 2045-2322 | - |
dc.identifier.uri | https://scholarworks.bwise.kr/erica/handle/2021.sw.erica/16510 | - |
dc.description.abstract | North Pacific subtropical high (NPSH) is permanent high-pressure system over the Northern Pacific Ocean and it extends to the western North Pacific during the boreal summer (June-July-August), which is so called the western North Pacific subtropical high (WNPSH). Here, we examine the covariability of the NPSH-WNPSH during summer using both observation and Coupled Model Intercomparison Project phase 5 (CMIP5) model data. The statistical analyses indicate that the NPSH-WNPSH covariability shows significant decadal variability in the observations, in addition, the in-phase relationship of NPSH-WNPSH is enhanced after the mid-to-late 1990s. A dipole-like sea surface temperature (SST) pattern, i.e., a warming in the western Pacific and a cooling in the eastern Pacific, is dominant after the mid-to-late 1990s, which acts to enhance the covariability of NPSH-WNPSH by modulating the atmospheric teleconnections. However, the covariability of NPSH-WNPSH in the future climate is not much influenced by the anthropogenic forcing but it is largely characterized by the natural decadal-to-interdecadal variability, implying that the enhancement of NPSH-WNPSH covariability after the mid-to-late 1990s could be considered as part of decadal-to-interdecadal variability. | - |
dc.language | 영어 | - |
dc.language.iso | en | - |
dc.publisher | Nature Publishing Group | - |
dc.title | Covariability of western tropical Pacific-North Pacific atmospheric circulation during summer | - |
dc.type | Article | - |
dc.contributor.affiliatedAuthor | Yeh, Sang-Wook | - |
dc.identifier.doi | 10.1038/srep16980 | - |
dc.identifier.scopusid | 2-s2.0-84948178983 | - |
dc.identifier.wosid | 000365091400001 | - |
dc.identifier.bibliographicCitation | Scientific Reports, v.5, pp.1 - 7 | - |
dc.relation.isPartOf | Scientific Reports | - |
dc.citation.title | Scientific Reports | - |
dc.citation.volume | 5 | - |
dc.citation.startPage | 1 | - |
dc.citation.endPage | 7 | - |
dc.type.rims | ART | - |
dc.type.docType | Article | - |
dc.description.journalClass | 1 | - |
dc.description.isOpenAccess | N | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.relation.journalResearchArea | Science & Technology - Other Topics | - |
dc.relation.journalWebOfScienceCategory | Multidisciplinary Sciences | - |
dc.subject.keywordPlus | NINO SOUTHERN-OSCILLATION | - |
dc.subject.keywordPlus | EL-NINO | - |
dc.subject.keywordPlus | INTERANNUAL VARIABILITY | - |
dc.subject.keywordPlus | CLIMATE | - |
dc.subject.keywordPlus | MONSOON | - |
dc.subject.keywordPlus | ENSO | - |
dc.subject.keywordPlus | PREDICTABILITY | - |
dc.subject.keywordPlus | PRECIPITATION | - |
dc.subject.keywordPlus | PATTERNS | - |
dc.subject.keywordPlus | IMPACT | - |
dc.identifier.url | https://www.nature.com/articles/srep16980 | - |
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