2026-05-26T11:39:22Zhttp://doidb.wdc-terra.org/oaip/oai
oai:doidb.wdc-terra.org:63522025-08-26T11:47:43ZDOIDBDOIDB.GIPP
false4DOIDB.GIPP 10.5880/GIPP.201303.1 Köhler, Andreas Andreas Köhler 0000-0002-1060-7637 Institutt for geofag, Universitetet i Oslo, Oslo, Norway Weidle, Christian Christian Weidle 0000-0002-3864-2979 Institut für Geowissenschaften, Christian-Albrechts-Universität zu Kiel, Kiel Germany Nuth, Christopher Christopher Nuth 0000-0002-1063-2832 Institutt for geofag, Universitetet i Oslo, Oslo, Norway Seismic Monitoring of Glacier Activity on Svalbard (SEISMOGLAC) - Datasets GFZ Data Services 2017 Icequakes Glacier monitoring cryo-seismology PASSIVE_SEISMIC > NETWORK SENSOR > GEOPHONE SENSOR > 3-C LAND EARTH SCIENCE > SOLID EARTH EARTH SCIENCE > SOLID EARTH > TECTONICS > EARTHQUAKES In Situ Land-based Platforms > GEOPHYSICAL STATIONS/NETWORKS Geophysical Instrumentation Pool Potsdam (GIPP) GFZ German Research Centre for Geosciences, Potsdam, Germany GIPP Support Team GFZ German Research Centre for Geosciences, Potsdam, Germany 2013-05/2013-09 Dataset 10.2312/GFZ.b103-17094 CC BY 4.0 Climatic change is of incredible importance in the polar regions as ice-sheets and glaciers respond strongly to change in average temperature. The analysis of seismic signals (icequakes) emitted by glaciers (i.e., cryo-seismology) is thus gaining importance as a tool for monitoring glacier activity. To understand the scaling relation between regional glacier-related seismicity and actual small-scale local glacier dynamics and to calibrate the identified classes of icequakes to locally observed waveforms, a temporary passive seismic monitoring experiment was conducted in the vicinity of the calving front of Kronebreen, one of the fastest tidewater glaciers on Svalbard (Fig. 1). By combining the local observations with recordings of the nearby GEOFON station GE.KBS, the local experiment provides an ideal link between local observations at the glacier to regional scale monitoring of NW Spitsbergen. During the 4-month operation period from May to September 2013, eight broadband seismometers and three 4-point short-period arrays were operating around the glacier front of Kronebreen.
Study area 12.5 78.8833 Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ https://doi.org/10.13039/501100010956 GIPP201303 Geophysical Instrumentation Pool Potsdam (GIPP) GIPP201303