2026-06-10T06:10:28Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:66492025-08-26T11:56:23ZDOIDBDOIDB.GIPPfalse4DOIDB.GIPP
10.5880/GIPP.201604.1
Köhler, Andreas
Andreas
Köhler
0000-0002-1060-7637
Institutt for geofag, Universitetet i Oslo, Oslo, Norway
Weidle, Christian
Christian
Weidle
0000-0002-3864-2979
Christian-Albrechts-Universität zu Kiel, Kiel, Germany
Nuth, Christopher
Christopher
Nuth
0000-0002-1063-2832
Institutt for geofag, Universitetet i Oslo, Oslo, Norway
Glacier dynamic ice loss quantified through seismic eyes (CALVINGSEIS) – Datasets
GFZ Data Services
2019
icequakes
glacier monitoring
cryo-seismology
PASSIVE_SEISMIC > NETWORK
SENSOR > GEOPHONE
SENSOR > 3-C
LAND
MINISEED_DATA_FORMAT
SEISMIC_WAVEFORM_DATA
EARTH SCIENCE > SOLID EARTH
EARTH SCIENCE > SOLID EARTH > GEOMORPHIC LANDFORMS/PROCESSES > GLACIAL PROCESSES
EARTH SCIENCE > SOLID EARTH > TECTONICS > EARTHQUAKES
In Situ Land-based Platforms > GEOPHYSICAL STATIONS/NETWORKS
Geophysical Instrumentation Pool Potsdam (GIPP)
GIPP Support Team
GFZ German Research Centre for Geosciences, Potsdam, Germany
2016-04-10/2016-09-04
2016-08-24/2016-09-03
Dataset
10.2312/GFZ.b103-19038
10.5194/esurf-7-1-2019
10.1017/aog.2019.15
10.1002/2016GL070589
CC BY-SA 4.0
Glacial contribution to eustatic sea level rise is currently dominated by loss of the smaller glaciers
and ice caps, about 40% of which are tidewater glaciers that lose mass through calving ice bergs.
The most recent predictions of glacier contribution to sea level rise over the next century are
strongly dependent upon models that are able to project individual glacier mass changes globally
and through time. A relatively new promising technique for monitoring glacier calving is through the
use of passive seismology. CalvingSEIS aims to produce high temporal resolution, continuous
calving records for the glaciers in Kongsfjord, Svalbard, and in particular for the Kronebreen glacier
laboratory through innovative, multi-disciplinary monitoring techniques combining fields of
seismology and bioacoustics to detect and locate individual calving events autonomously and
further to develop methods for the quantification of calving ice volumes directly from the seismic
and acoustic signals.
CalvingSEIS survey (April to September 2016)
11.7884
11.9421
78.9145
78.9399
CalvingSEIS survey (August to September 2016)
12.3388
12.5399
78.8644
78.8975
Geophysical Instrument Pool Potsdam
201604
Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ
http://doi.org/10.13039/501100010956