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The influence of the Drygalski Ice Tongue on the local ocean

Cited 11 time in wos
Cited 13 time in scopus

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dc.contributor.authorCraig Stevens-
dc.contributor.authorHwang, Chung Yeon-
dc.contributor.authorNatalie Robinson-
dc.contributor.authorBrett Grant-
dc.contributor.authorYun, Sukyoung-
dc.contributor.authorGiannetta Fusco-
dc.contributor.authorLee, Won Sang-
dc.coverage.spatialAntarctica-
dc.coverage.spatialDrygalski Glacier-
dc.coverage.spatialEast Antarctica-
dc.coverage.spatialRoss Sea-
dc.coverage.spatialSouthern Ocean-
dc.coverage.spatialVictoria Land-
dc.coverage.spatialDrygalski Ice Tongue-
dc.date.accessioned2018-03-20T13:39:54Z-
dc.date.available2018-03-20T13:39:54Z-
dc.date.issued2017-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/6067-
dc.description.abstractThe Drygalski Ice Tongue presents an ∼80 km long floating obstacle to alongshore flows in the Victoria Land coastal ocean region of the Western Ross Sea. Here we use oceanographic data from near to the tongue to explore the interplay between the floating glacier and the local currents and stratification. A vessel-based circuit of the glacier, recording ocean temperature and salinity profiles, reveals the southwest corner to be the coldest and most complex in terms of vertical structure. The southwest corner structure beneath the surface warm, salty layer sustains a block of very cold water extending to 200 m depth. In this same location there was a distinct layer at 370 m not seen anywhere else of water at ∼?1.93°C. The new observations broadly, but not directly, support the presence of a coherent Victoria Land Coastal Current. The data suggest the northward moving coastal current turns against the Coriolis force and works its way anticlockwise around the glacier, but with leakage beneath the glacier through the highly 'rippled' underside, resulting in a spatially heterogeneous supply to the Terra Nova Bay Polynya region ? an important location for the formation of high-salinity shelf water.-
dc.languageEnglish-
dc.subjectPhysical Geography-
dc.subjectGeology-
dc.titleThe influence of the Drygalski Ice Tongue on the local ocean-
dc.title.alternative드라이갈스키 빙설이 주변 연안 해양에 미치는 영향 연구-
dc.typeArticle-
dc.identifier.bibliographicCitationCraig Stevens, et al. 2017. "The influence of the Drygalski Ice Tongue on the local ocean". <em>ANNALS OF GLACIOLOGY</em>, 58(74): 51-59.-
dc.citation.titleANNALS OF GLACIOLOGY-
dc.citation.volume58-
dc.citation.number74-
dc.identifier.doi10.1017/aog.2017.4-
dc.citation.startPage51-
dc.citation.endPage59-
dc.description.articleClassificationSCIE-
dc.description.jcrRateJCR 2015:54.348-
dc.subject.keywordDrygalski Ice Tongue-
dc.subject.keywordOcean-Ice interaction-
dc.subject.keywordPhysical oceanography-
dc.identifier.localId2017-0101-
dc.identifier.scopusid2-s2.0-85026760241-
dc.identifier.wosid000416835100007-
Appears in Collections  
2014-2018, Investigating Cryospheric Evolution of the Victoria Land, Antarctica -ICE- (14-18) / Lee, Won Sang (PM14020; PM15020; PM16020; PM17020)
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