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Characteristics of internal variability on summer rainfall in Northeast Asia in a changing climate

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dc.contributor.authorHyun, Seung-Hwon-
dc.contributor.authorYeh, Sang-Wook-
dc.date.accessioned2021-06-22T09:08:53Z-
dc.date.available2021-06-22T09:08:53Z-
dc.date.created2021-01-21-
dc.date.issued2020-01-
dc.identifier.issn0930-7575-
dc.identifier.urihttps://scholarworks.bwise.kr/erica/handle/2021.sw.erica/1386-
dc.description.abstractUsing a 35-ensemble member simulated with the community earth system model-large ensemble (CESM-LE) experiment, we examined the characteristics of internal variability (IV) on the Northeast Asian summer rainfall anomaly (NASRA) in a changing climate. The NASRA, which is defined as the rainfall anomaly averaged across Northeast Asia (30 degrees-40 degrees N, 115 degrees-145 degrees E), consists of the tropics-related rainfall anomaly and the extratropics-related rainfall anomaly. In this study, the IV was estimated by the spread of rainfall simulated in each ensemble member from their ensemble mean. The IV associated with the tropics-related rainfall variability did not change significantly from the present climate to a future climate. In contrast, the IV associated with the NASRA gradually increased from the mid-twenty first century and this was mostly due to an increase of IV associated with the extratropics-related rainfall variability. This implies that the predictability of NASRA may decrease in a future changing climate because of the extratropics-related rainfall variability associated with zonal atmospheric wave train patterns including Eurasian-like pattern, Silk Road pattern or Circumglobal Teleconnection pattern. We also discussed the characteristic change of IV associated with the tropics-related and the extratropics-related rainfall variability in a future warmer climate.-
dc.language영어-
dc.language.isoen-
dc.publisherSpringer Verlag-
dc.titleCharacteristics of internal variability on summer rainfall in Northeast Asia in a changing climate-
dc.typeArticle-
dc.contributor.affiliatedAuthorYeh, Sang-Wook-
dc.identifier.doi10.1007/s00382-019-05051-1-
dc.identifier.scopusid2-s2.0-85076118656-
dc.identifier.wosid000500679100002-
dc.identifier.bibliographicCitationClimate Dynamics, v.54, no.1-2, pp.1179 - 1195-
dc.relation.isPartOfClimate Dynamics-
dc.citation.titleClimate Dynamics-
dc.citation.volume54-
dc.citation.number1-2-
dc.citation.startPage1179-
dc.citation.endPage1195-
dc.type.rimsART-
dc.type.docTypeArticle-
dc.description.journalClass1-
dc.description.isOpenAccessN-
dc.description.journalRegisteredClassscie-
dc.description.journalRegisteredClassscopus-
dc.relation.journalResearchAreaMeteorology & Atmospheric Sciences-
dc.relation.journalWebOfScienceCategoryMeteorology & Atmospheric Sciences-
dc.subject.keywordPlusPACIFIC ANOMALOUS ANTICYCLONE-
dc.subject.keywordPlusEL-NINO-
dc.subject.keywordPlusINTERANNUAL VARIABILITY-
dc.subject.keywordPlusINDIAN-OCEAN-
dc.subject.keywordPlusTELECONNECTION PATTERN-
dc.subject.keywordPlusNORTHWEST PACIFIC-
dc.subject.keywordPlusCOMBINATION-MODE-
dc.subject.keywordPlusFUTURE CHANGES-
dc.subject.keywordPlusSST ANOMALIES-
dc.subject.keywordPlusMONSOON-
dc.identifier.urlhttps://link.springer.com/article/10.1007/s00382-019-05051-1-
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