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Glacier calving can cause violent tsunami waves which, upon landfall, cancause severe destruction. Here we present data acquired during a calvingevent from Eqip Sermia, an ocean-terminating glacier in west Greenland.During an exceptionally well-documented event, the collapse of 9  ×  105 m3ice from a 200 m high ice cliff caused a tsunami wave of 50 m height, traveling at a speed of25–33 m s−1. This wave was filmed from a tour boat at800 m distance from the calving face, and simultaneously measuredwith a terrestrial radar interferometer and a tide gauge. Tsunami wave run-upheight on the steep opposite shore at a distance of 4 km was10–15 m, destroying infrastructure and eroding oldvegetation. These observations indicate that such high tsunami waves area recent phenomenon in the history of this glacier. Analysis of the datashows that only moderately bigger tsunami waves are to be expected in thefuture, even under rather extreme scenarios

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