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Elastic uplift in southeast Greenland due to rapid ice mass loss
Ist Teil von
Geophysical research letters, 2007-11, Vol.34 (21), p.L21701-n/a
Ort / Verlag
Washington, DC: American Geophysical Union
Erscheinungsjahr
2007
Link zum Volltext
Quelle
Wiley Online Library - AutoHoldings Journals
Beschreibungen/Notizen
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.