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How does the SST variability over the western North AtlanticOcean control Arctic warming over the Barents?Kara Seas?

Cited 27 time in wos
Cited 29 time in scopus

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DC Field Value Language
dc.contributor.authorOk Jung-
dc.contributor.authorKim, Baek-Min-
dc.contributor.authorJee-Hoon Jeong-
dc.contributor.authorBaek, Eun-Hyuk-
dc.contributor.authorKim, Seong-Joong-
dc.contributor.authorYoung-Kwon Lim-
dc.contributor.authorKazutoshi Sato-
dc.contributor.authorMi-Kyung Sung-
dc.coverage.spatialArctic Ocean-
dc.coverage.spatialAtlantic Ocean-
dc.coverage.spatialAtlantic Ocean-
dc.coverage.spatialBarents Sea-
dc.coverage.spatialKara Sea-
dc.date.accessioned2018-03-20T13:38:53Z-
dc.date.available2018-03-20T13:38:53Z-
dc.date.issued2017-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/6043-
dc.description.abstractArctic warming over the Barents?Kara Seas and its impacts on the mid-latitude circulations have been widely discussed. However, the specific mechanism that brings the warming still remains unclear. In this study, a possible cause of the regional Arctic warming over the Barents?Kara Seas during early winter (October?December) is suggested. We found that warmer sea surface temperature anomalies over the western North Atlantic Ocean (WNAO) modulate the transient eddies overlying the oceanic frontal region. The altered transient eddy vorticity flux acts as a source for the Rossby wave straddling the western North Atlantic and the Barents?Kara Seas (Scandinavian pattern), and induces a significant warm advection, increasing surface and lowerlevel temperature over the Eurasian sector of the Arctic Ocean. The importance of the sea surface temperature anomalies over the WNAO and subsequent transient eddy forcing over the WNAO was also supported by both specially designed simple model experiments and general circulation model experiments.-
dc.languageEnglish-
dc.subjectEnvironmental Sciences & Ecology-
dc.subjectMeteorology & Atmospheric Sciences-
dc.titleHow does the SST variability over the western North AtlanticOcean control Arctic warming over the Barents?Kara Seas?-
dc.title.alternative북서대서양의 해수면 온도 변동이 바렌츠-카라 해역의 북극 온난화에 미치는 영향-
dc.typeArticle-
dc.identifier.bibliographicCitationOk Jung, et al. 2017. "How does the SST variability over the western North AtlanticOcean control Arctic warming over the Barents?Kara Seas?". <em>ENVIRONMENTAL RESEARCH LETTERS</em>, 12(3): 1-8.-
dc.citation.titleENVIRONMENTAL RESEARCH LETTERS-
dc.citation.volume12-
dc.citation.number3-
dc.identifier.doi10.1088/1748-9326/aa5f3b-
dc.citation.startPage1-
dc.citation.endPage8-
dc.description.articleClassificationSCIE-
dc.description.jcrRateJCR 2015:12.444-
dc.subject.keywordArctic warming-
dc.subject.keywordStationary Wave Model-
dc.subject.keywordWestern North Atlantic Ocean-
dc.subject.keywordtransient eddy vorticity forcing-
dc.identifier.localId2017-0037-
dc.identifier.scopusid2-s2.0-85028505321-
dc.identifier.wosid000397803200001-
Appears in Collections  
2017-2018, Development and Application of the Korea Polar Prediction System (KPOPS) for Climate Change and Disasterous Weather Events (17-18) / Kim, Baek-Min (PE17130; PE18130)
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