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 62N and 66N. Citation: Khan, 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.
- Global warming
- Ice mass loss
Khan, S. A., Van dam, T., Hamilton, G. S., Stearns, L. A., Wahr, J., Larson, K. M., & Francis, O. (2007). Elastic uplift in southeast Greenland due to rapid ice mass loss. Geophysical Research Letters, 34. https://doi.org/10.1029/2007/GL031468