Articles | Volume 10, issue 3
Research article
12 May 2016
Research article |  | 12 May 2016

Multi-method observation and analysis of a tsunami caused by glacier calving

Martin P. Lüthi and Andreas Vieli

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Cited articles

Amundson, J. M., Truffer, M., Lüthi, M. P., Fahnestock, M., Motyka, R. J., and West, M.: Glacier, fjord, and seismic response to recent large calving events, Jakobshavn Isbræ, Greenland, Geophys. Res. Lett., 35, L22501,, 2008.
Amundson, J. M., Fahnestock, M., Truffer, M., Brown, J., Lüthi, M., and Motyka, R.: Ice mélange dynamics and implications for terminus stability, Jakobshavn Isbræ, Greenland, J. Geophys. Res., 115, F01005,, 2010.
Amundson, J. M., Clinton, J. F., Fahnestock, M., Truffer, M., Lüthi, M. P., and Motyka, R. J.: Observing calving-generated ocean waves with coastal broadband seismometers, Jakobshavn Isbræ, Greenland, Ann. Glaciol., 60, 79–84,, 2012.
Bauer, A.: Glaciologie Groenland II. Le glacier de l'Eqe. 6, Tech. rep., Expéditions Polaires Francaises, Hermann, Paris, 118 pp., 1955.
Bauer, A.: Le glacier de l'Eqe (Eqip Sermia). Mouvement et variations du front (1959), Tech. Rep. 2, Expédition glaciologique internationale au Groenland (EGIG), Meddelelser om Grønland, Reitzel, København, 1968.
Short summary
Glaciers flowing into the ocean sometimes release huge pieces of ice and cause violent tsunami waves which, upon landfall, can cause severe destruction. During an exceptionally well-documented event at Eqip Sermia, west Greenland, the collapse of a 200 m high ice cliff caused a tsunami wave of 50 m height, traveling at a speed exceeding 100 km h−1. This tsunami wave was filmed from a tour boat, and was simultaneously observed with several instruments, as was the run-up of 15 m on the shore.