Articles | Volume 15, issue 1
https://doi.org/10.5194/tc-15-283-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-15-283-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Passive seismic recording of cryoseisms in Adventdalen, Svalbard
Department of Geosciences, University of Tromsø – The Arctic
University of Norway, 9037 Tromsø, Norway
Research Centre for Arctic Petroleum Exploration (ARCEx), 9037 Tromsø, Norway
Alfred Hanssen
Department of Geosciences, University of Tromsø – The Arctic
University of Norway, 9037 Tromsø, Norway
Research Centre for Arctic Petroleum Exploration (ARCEx), 9037 Tromsø, Norway
Bent Ole Ruud
Research Centre for Arctic Petroleum Exploration (ARCEx), 9037 Tromsø, Norway
Department of Earth Science, University of Bergen, 5007 Bergen, Norway
Helene Meling Stemland
Research Centre for Arctic Petroleum Exploration (ARCEx), 9037 Tromsø, Norway
Department of Earth Science, University of Bergen, 5007 Bergen, Norway
Tor Arne Johansen
Research Centre for Arctic Petroleum Exploration (ARCEx), 9037 Tromsø, Norway
Department of Earth Science, University of Bergen, 5007 Bergen, Norway
The University Centre in Svalbard (UNIS), 9171 Longyearbyen, Norway
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We have investigated a long-term record of ground vibrations, recorded by a seismic array installed in Adventdalen, Svalbard. This record contains a large number of
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Short summary
A series of unusual ground motion signatures were identified in geophone recordings at a frost polygon site in Adventdalen on Svalbard. By analysing where the ground motion originated in time and space, we are able to classify them as cryoseisms, also known as frost quakes, a ground-cracking phenomenon that occurs as a result of freezing processes. The waves travelling through the ground produced by these frost quakes also allow us to measure the structure of the permafrost in the near surface.
A series of unusual ground motion signatures were identified in geophone recordings at a frost...