KOPRI Repository

Configuration of the Northern Antarctic Peninsula Ice Sheet at LGM based on a new synthesis of seabed imagery

Cited 23 time in wos
Cited 24 time in scopus
Metadata Downloads

Full metadata record

DC FieldValueLanguage
dc.contributor.authorC. Lavoie-
dc.contributor.authorD. Amblas-
dc.contributor.authorJ. B. Anderson-
dc.contributor.authorM. Canals-
dc.contributor.authorJ. Wellner-
dc.contributor.authorJ. Gutt-
dc.contributor.authorYoo, Kyu-Cheul-
dc.contributor.authorH.-W. Schenke-
dc.contributor.authorR. D. Larter-
dc.contributor.authorT. A. Scambos-
dc.contributor.authorE. C. Pettit-
dc.contributor.authorE. W. Domack-
dc.date.accessioned2018-03-29T06:04:52Z-
dc.date.available2018-03-29T06:04:52Z-
dc.date.issued2015-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/7334-
dc.description.abstractWe present a new seafloor map for the northern Antarctic Peninsula (AP), including swath multibeam data sets from five national programs. Our map allows for the examination and interpretation of Last Glacial Maximum (LGM) paleo-ice-flow paths developed on the seafloor from the preservation of mega-scale glacial lineations, drumlinized features, and selective linear erosion. We combine this with terrestrial observations of flow direction to place constraints on ice divides and ice domes on the AP continental shelf during the LGM time interval. The results show a flow bifurcation as ice exits the Larsen B embayment. Flow emanating off the Seal Nunataks (including Robertson Island) is directed toward the southeast, then eastward as the flow transits toward the Robertson Trough. A second, stronger "streaming flow" is directed toward the southeast, then southward as ice overflowed the tip of the Jason Peninsula to reach the southern perimeter of the embayment. Our reconstruction also refines the extent of at least five other distinct paleo-ice-stream systems that, in turn, serve to delineate seven broad regions where contemporaneous ice domes must have been centered on the continental shelf at LGM. Our reconstruction is more detailed than other recent compilations because we followed specific ice-flow indicators and have kept tributary flow paths parallel.-
dc.languageEnglish-
dc.titleConfiguration of the Northern Antarctic Peninsula Ice Sheet at LGM based on a new synthesis of seabed imagery-
dc.title.alternative새로운 해저 이미지를 기반으로 지난최대빙하기에 북부 남극반도 빙상 실현-
dc.typeArticle-
dc.identifier.bibliographicCitationC. Lavoie, et al. 2015. "Configuration of the Northern Antarctic Peninsula Ice Sheet at LGM based on a new synthesis of seabed imagery". <em>CRYOSPHERE</em>, 9: 613-629.-
dc.citation.titleCRYOSPHERE-
dc.citation.volume9-
dc.identifier.doi10.5194/tc-9-613-2015-
dc.citation.startPage613-
dc.citation.endPage629-
dc.description.articleClassificationSCIE-
dc.description.jcrRateJCR 2013:6.321839080459771-
dc.identifier.localId2015-0027-
dc.identifier.scopusid2-s2.0-84926430069-
dc.identifier.wosid000353878400014-
Appears in Collections  
2014-2016, Monitoring of Abrupt Environmental Change in The Ice Shelf System and Reconstruction of Quaternary Deglaciation History in West Antarctica (14-16) / Yoon; Ho Il
Files in This Item
General Conditions
      ROMEO Green
    Can archive pre-print and post-print or publisher's version/PDF
      ROMEO Blue
    Can archive post-print (ie final draft post-refereeing) or publisher's version/PDF
      ROMEO Yellow
    Can archive pre-print (ie pre-refereeing)
      ROMEO White
    Archiving not formally supported

    Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.

    Browse