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Sensitivity of Pine Island Glacier to observed ocean forcing

Cited 55 time in wos
Cited 57 time in scopus

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dc.contributor.authorKim, Tae-Wan-
dc.contributor.authorKaren J. Heywood-
dc.contributor.authorSridhar Anandakrishnan-
dc.contributor.authorE. Povl Abrahamsen-
dc.contributor.authorDavid E. Shean-
dc.contributor.authorRichard B. Alley-
dc.contributor.authorIan R. Joughin-
dc.contributor.authorByron R. Parizek-
dc.contributor.authorPierre Dutrieux-
dc.contributor.authorMitchell Bushuk-
dc.contributor.authorKnut Christianson-
dc.contributor.authorDavid M. Holland-
dc.contributor.authorRobert Bindschadler-
dc.contributor.authorStan Jacobs-
dc.contributor.authorAdrian Jenkins-
dc.contributor.authorBenjamin G. M. Webber-
dc.contributor.authorMartin Truffer-
dc.contributor.authorTim Stanton-
dc.contributor.authorKeith Nicholls-
dc.contributor.authorLee, Sang H.-
dc.date.accessioned2018-03-29T06:14:57Z-
dc.date.available2018-03-29T06:14:57Z-
dc.date.issued2016-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/7506-
dc.description.abstractWe present subannual observations (2009?2014) of a major West Antarctic glacier (Pine Island Glacier) and the neighboring ocean. Ongoing glacier retreat and accelerated ice flow were likely triggered a few decades ago by increased ocean-induced thinning, which may have initiated marine ice sheet instability. Following a subsequent 60% drop in ocean heat content from early 2012 to late 2013, ice flow slowed, but by-
dc.languageKorean-
dc.titleSensitivity of Pine Island Glacier to observed ocean forcing-
dc.title.alternative관측된 해양기원 힘들에 의한 Pine Island 빙붕의 민감도-
dc.typeArticle-
dc.identifier.bibliographicCitationKim, Tae-Wan, et al. 2016. "Sensitivity of Pine Island Glacier to observed ocean forcing". <em>GEOPHYSICAL RESEARCH LETTERS</em>, 43(20): 10817-10825.-
dc.citation.titleGEOPHYSICAL RESEARCH LETTERS-
dc.citation.volume43-
dc.citation.number20-
dc.identifier.doi10.1002/2016GL070500-
dc.citation.startPage10817-
dc.citation.endPage10825-
dc.description.articleClassificationSCI-
dc.description.jcrRateJCR 2014:5.142-
dc.subject.keywordGrounded ice speed slowed by only~1% despite ~60% drop in ocean heatcontent-
dc.subject.keywordIce speed recovered after thecold-ocean anomaly ended-
dc.subject.keywordPine Island Glacier speed is correlatedwith ocean temperature-
dc.identifier.localId2016-0260-
dc.identifier.scopusid2-s2.0-84995618138-
dc.identifier.wosid000388293800045-
Appears in Collections  
2014-2016, Physical and Bio-Geochemical Processes in the Amundsen Sea / Lee; Sang H. (PP15020; PP16020; PP14020)
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