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Step-wise changes in glacier flow speed coincide with calving and
glacial earthquakes at Helheim Glacier, Greenland
Full citation: Nettles, M., T. B. Larsen, P. Elósegui, G. S. Hamilton, L. A. Stearns, A. P. Ahlstrøm, J. L. Davis, M. L. Andersen, J. de Juan, S. A. Khan, L. Stenseng, G. Ekström, and R. Forsberg (2008), Step-wise changes in glacier flow speed coincide with calving and glacial earthquakes at Helheim Glacier, Greenland, Geophys. Res. Lett., 35, L24503, doi:10.1029/2008GL036127.
Abstract
Geodetic observations show several large, sudden increases in flow speed at Helheim Glacier, one of GreenlandŐs largest outlet glaciers, during summer, 2007. These step-like accelerations, detected along the length of the glacier, coincide with teleseismically detected glacial earthquakes and major iceberg calving events. No coseismic offset in the position of the glacier surface is observed; instead, modest tsunamis associated with the glacial earthquakes implicate glacier calving in the seismogenic process. Our results link changes in glacier velocity directly to calving-front behavior at GreenlandŐs largest outlet glaciers, on timescales as short as minutes to hours, and clarify the mechanism by which glacial earthquakes occur.
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