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dc.contributor.authorKhan, Shfaqat Abbas
dc.contributor.authorWahr, John
dc.contributor.authorStearns, Leigh A.
dc.contributor.authorHamilton, Gordon S.
dc.contributor.authorvan Dam, Tonie
dc.contributor.authorLarson, Kristine M.
dc.contributor.authorFrancis, Olivier
dc.date.accessioned2015-03-24T21:20:37Z
dc.date.available2015-03-24T21:20:37Z
dc.date.issued2007-11-01
dc.identifier.citationKhan, S. A., J. Wahr, L. A. Stearns, G. S. Hamilton, T. van Dam, K. M. Larson, and O. Francis (2007), Elastic uplift in southeast Greenland due to rapid ice mass loss, Geophys. Res. Lett., 34, L21701. http://www.dx.doi.org/10.1029/2007GL031468en_US
dc.identifier.issn0094-8276
dc.identifier.urihttp://hdl.handle.net/1808/17213
dc.descriptionThis is the publisher's version, also available electronically from "http://onlinelibrary.wiley.com".en_US
dc.description.abstract[1] The rapid unloading of ice from the southeastern sector of the Greenland ice sheet between 2001 and 2006 caused an elastic uplift of ∼35 mm at a GPS site in Kulusuk. Most of the uplift results from ice dynamic-induced volume losses on two nearby outlet glaciers. Volume loss from Helheim Glacier, calculated from sequential digital elevation models, contributes about ∼16 mm of the observed uplift, with an additional ∼5 mm from volume loss of Kangerdlugssuaq Glacier. The remaining uplift signal is attributed to significant melt-induced ice volume loss from the ice sheet margin along the southeast coast between 62°N and 66°N.en_US
dc.publisherAmerican Geophysical Unionen_US
dc.subjectice mass lossen_US
dc.subjectGPSen_US
dc.subjectelastic upliften_US
dc.titleElastic uplift in southeast Greenland due to rapid ice mass lossen_US
dc.typeArticle
kusw.kuauthorStearns, Leigh
kusw.kudepartmentGeologyen_US
dc.identifier.doi10.1029/2007GL031468
kusw.oaversionScholarly/refereed, publisher version
kusw.oapolicyThis item does not meet KU Open Access policy criteria.
dc.rights.accessrightsopenAccess


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