Khan, Shfaqat AbbasWahr, JohnStearns, Leigh A.Hamilton, Gordon S.van Dam, TonieLarson, Kristine M.Francis, Olivier2015-03-242015-03-242007-11-01Khan, 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/10.1029/2007GL0314680094-8276https://hdl.handle.net/1808/17213This is the publisher's version, also available electronically from "http://onlinelibrary.wiley.com".[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.ice mass lossGPSelastic upliftArticle10.1029/2007GL031468openAccess