Multi-method observation and analysis of a tsunami caused by glacier calving
Glacier calving can cause violent tsunami waves which, upon landfall, can cause severe destruction. Here we present data acquired during a calving event from Eqip Sermia, an ocean-terminating glacier in west Greenland. During an exceptionally well-documented event, the collapse of 9 × 105 m3 ice fro...
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ftunivzuerich:oai:www.zora.uzh.ch:124771 2024-09-09T19:41:22+00:00 Multi-method observation and analysis of a tsunami caused by glacier calving Lüthi, Martin P Vieli, Andreas 2016 application/pdf https://www.zora.uzh.ch/id/eprint/124771/ https://www.zora.uzh.ch/id/eprint/124771/1/2016_Luethi%26Vieli2016.pdf https://doi.org/10.5167/uzh-124771 https://doi.org/10.5194/tc-10-995-2016 eng eng Copernicus Publications https://www.zora.uzh.ch/id/eprint/124771/1/2016_Luethi%26Vieli2016.pdf doi:10.5167/uzh-124771 doi:10.5194/tc-10-995-2016 urn:issn:1994-0416 info:eu-repo/semantics/openAccess Lüthi, Martin P; Vieli, Andreas (2016). Multi-method observation and analysis of a tsunami caused by glacier calving. The Cryosphere, 10(3):995-1002. Institute of Geography 910 Geography & travel Earth-Surface Processes Water Science and Technology Journal Article PeerReviewed info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2016 ftunivzuerich https://doi.org/10.5167/uzh-12477110.5194/tc-10-995-2016 2024-08-21T00:19:55Z Glacier calving can cause violent tsunami waves which, upon landfall, can cause severe destruction. Here we present data acquired during a calving event from Eqip Sermia, an ocean-terminating glacier in west Greenland. During an exceptionally well-documented event, the collapse of 9 × 105 m3 ice from a 200 m high ice cliff caused a tsunami wave of 50 m height, traveling at a speed of 25–33 m s−1 . This wave was filmed from a tour boat at 800m distance from the calving face, and simultaneously measured with a terrestrial radar interferometer and a tide gauge. Tsunami wave run-up height on the steep opposite shore at a distance of 4 km was 10–15 m, destroying infrastructure and eroding old vegetation. These observations indicate that such high tsunami waves are a recent phenomenon in the history of this glacier. Analysis of the data shows that only moderately bigger tsunami waves are to be expected in the future, even under rather extreme scenarios. Article in Journal/Newspaper glacier Greenland The Cryosphere University of Zurich (UZH): ZORA (Zurich Open Repository and Archive Greenland Eqip Sermia ENVELOPE(-50.067,-50.067,69.817,69.817) |
institution |
Open Polar |
collection |
University of Zurich (UZH): ZORA (Zurich Open Repository and Archive |
op_collection_id |
ftunivzuerich |
language |
English |
topic |
Institute of Geography 910 Geography & travel Earth-Surface Processes Water Science and Technology |
spellingShingle |
Institute of Geography 910 Geography & travel Earth-Surface Processes Water Science and Technology Lüthi, Martin P Vieli, Andreas Multi-method observation and analysis of a tsunami caused by glacier calving |
topic_facet |
Institute of Geography 910 Geography & travel Earth-Surface Processes Water Science and Technology |
description |
Glacier calving can cause violent tsunami waves which, upon landfall, can cause severe destruction. Here we present data acquired during a calving event from Eqip Sermia, an ocean-terminating glacier in west Greenland. During an exceptionally well-documented event, the collapse of 9 × 105 m3 ice from a 200 m high ice cliff caused a tsunami wave of 50 m height, traveling at a speed of 25–33 m s−1 . This wave was filmed from a tour boat at 800m distance from the calving face, and simultaneously measured with a terrestrial radar interferometer and a tide gauge. Tsunami wave run-up height on the steep opposite shore at a distance of 4 km was 10–15 m, destroying infrastructure and eroding old vegetation. These observations indicate that such high tsunami waves are a recent phenomenon in the history of this glacier. Analysis of the data shows that only moderately bigger tsunami waves are to be expected in the future, even under rather extreme scenarios. |
format |
Article in Journal/Newspaper |
author |
Lüthi, Martin P Vieli, Andreas |
author_facet |
Lüthi, Martin P Vieli, Andreas |
author_sort |
Lüthi, Martin P |
title |
Multi-method observation and analysis of a tsunami caused by glacier calving |
title_short |
Multi-method observation and analysis of a tsunami caused by glacier calving |
title_full |
Multi-method observation and analysis of a tsunami caused by glacier calving |
title_fullStr |
Multi-method observation and analysis of a tsunami caused by glacier calving |
title_full_unstemmed |
Multi-method observation and analysis of a tsunami caused by glacier calving |
title_sort |
multi-method observation and analysis of a tsunami caused by glacier calving |
publisher |
Copernicus Publications |
publishDate |
2016 |
url |
https://www.zora.uzh.ch/id/eprint/124771/ https://www.zora.uzh.ch/id/eprint/124771/1/2016_Luethi%26Vieli2016.pdf https://doi.org/10.5167/uzh-124771 https://doi.org/10.5194/tc-10-995-2016 |
long_lat |
ENVELOPE(-50.067,-50.067,69.817,69.817) |
geographic |
Greenland Eqip Sermia |
geographic_facet |
Greenland Eqip Sermia |
genre |
glacier Greenland The Cryosphere |
genre_facet |
glacier Greenland The Cryosphere |
op_source |
Lüthi, Martin P; Vieli, Andreas (2016). Multi-method observation and analysis of a tsunami caused by glacier calving. The Cryosphere, 10(3):995-1002. |
op_relation |
https://www.zora.uzh.ch/id/eprint/124771/1/2016_Luethi%26Vieli2016.pdf doi:10.5167/uzh-124771 doi:10.5194/tc-10-995-2016 urn:issn:1994-0416 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5167/uzh-12477110.5194/tc-10-995-2016 |
_version_ |
1809910773359575040 |