Recent recovery of the Siberian High intensity SCIE SCOPUS

DC Field Value Language
dc.contributor.author Jeong, Jee-Hoon -
dc.contributor.author Ou, Tinghai -
dc.contributor.author Linderholm, Hans W. -
dc.contributor.author Kim, Baek-Min -
dc.contributor.author Kim, Seong-Joong -
dc.contributor.author Kug, Jong-Seong -
dc.contributor.author Chen, Deliang -
dc.date.accessioned 2020-04-20T07:25:30Z -
dc.date.available 2020-04-20T07:25:30Z -
dc.date.created 2020-01-28 -
dc.date.issued 2011-12 -
dc.identifier.issn 0148-0227 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/3777 -
dc.description.abstract This study highlights the fast recovery of the wintertime Siberian High intensity (SHI) over the last two decades. The SHI showed a marked weakening trend from the 1970s to 1980s, leading to unprecedented low SHI in the early 1990s according to most observational data sets. This salient declining SHI trend, however, was sharply replaced by a fast recovery over the last two decades. Since the declining SHI trend has been considered as one of the plausible consequences of climate warming, the recent SHI recovery seemingly contradicts the continuous progression of climate warming in the Northern Hemisphere. We suggest that alleviated surface warming and decreased atmospheric stability in the central Siberia region, associated with an increase in Eurasian snow cover, in the recent two decades contributed to this rather unexpected SHI recovery. The prominent SHI change, however, is not reproduced by general circulation model (GCM) simulations used in the IPCC AR4. The GCMs indicate the steady weakening of the SHI for the entire 21st century, which is found to be associated with a decreasing Eurasian snow cover in the simulations. An improvement in predicting the future climate change in regional scale is desirable. -
dc.description.uri 1 -
dc.language English -
dc.publisher AMER GEOPHYSICAL UNION -
dc.title Recent recovery of the Siberian High intensity -
dc.type Article -
dc.citation.title JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES -
dc.citation.volume 116 -
dc.contributor.alternativeName 국종성 -
dc.identifier.bibliographicCitation JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, v.116 -
dc.identifier.doi 10.1029/2011JD015904 -
dc.identifier.scopusid 2-s2.0-82955177015 -
dc.identifier.wosid 000297654900001 -
dc.type.docType Article -
dc.description.journalClass 1 -
dc.description.isOpenAccess N -
dc.subject.keywordPlus SEA-LEVEL PRESSURE -
dc.subject.keywordPlus ASIAN WINTER MONSOON -
dc.subject.keywordPlus SNOW COVER -
dc.subject.keywordPlus ARCTIC OSCILLATION -
dc.subject.keywordPlus ATMOSPHERIC RESPONSE -
dc.subject.keywordPlus CLIMATE-CHANGE -
dc.subject.keywordPlus REANALYSIS -
dc.subject.keywordPlus VARIABILITY -
dc.subject.keywordPlus LAND -
dc.subject.keywordPlus ANOMALIES -
dc.relation.journalWebOfScienceCategory Meteorology & Atmospheric Sciences -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.relation.journalResearchArea Meteorology & Atmospheric Sciences -
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