2026-07-23T03:02:52Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:61392026-06-10T10:04:57ZDOIDBDOIDB.GIPPfalse4DOIDB.GIPP
10.5880/GIPP.201315.1
Overduin, Paul
Paul
Overduin
0000-0001-9849-4712
Periglacial Department, Alfred Wegener Institute Helmholtz-Center for Polar and Marine Research, Potsdam, Germany
Ryberg, Trond
Trond
Ryberg
0000-0001-7129-5596
GFZ German Research Centre for Geosciences, Potsdam, Germany
Kneier, Fabian
Fabian
Kneier
0000-0002-0474-0087
Periglacial Department, Alfred Wegener Institute Helmholtz-Center for Polar and Marine Research, Potsdam, Germany
Haberland, Christian
Christian
Haberland
0000-0002-2981-7087
GFZ German Research Centre for Geosciences, Potsdam, Germany
Grigoriev, Mikhail
Mikhail
Grigoriev
Siberian Branch-Russian Academy of Sciences, Mel’nikov Permafrost Institute, Yakutsk, Russia
Amphibious passive seismic recordings on and around Muostakh Island (Laptev Sea, Russia) in August/September 2013 - Datasets
Deutsches GeoForschungsZentrum GFZ
2015
Seismology
Laptev Sea (Russia)
Cryosphere
Solid Earth
Permafrost
PASSIVE_SEISMIC > NETWORK
SENSOR > GEOPHONE
SENSOR > 3-C
MARINE
MINISEED_DATA_FORMAT
SEISMIC_WAVEFORM_DATA
EARTH SCIENCE > CRYOSPHERE
EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > PERMAFROST
EARTH SCIENCE > SOLID EARTH
GIPP Support Team
GFZ German Research Centre for Geosciences, Potsdam, Germany
2013-08/2013-09
2017-09-01
2013-08/2013-09
Dataset
10.17815/jlsrf-2-128
CC BY 4.0
In August and September 2013, 17 shallow ocean bottom seismograph (S-OBS) stations and 8 land stations had been deployed on and around Muostakh Island (Laptev Sea, Russia) for a time period of 24 days.
The specifically designed underwater recording equipment consists of a low-power digital recorder, a standard 4.5Hz 3-component geophone, and a battery pack. These components are enclosed in a watertight cylindrical container safe for operation down to 100m water depth. Land stations were also equipped with 4.5 Hz 1C-geophones as well as with batteries. All instruments recorded continuously with 200 samples per second (sps). The stations were deployed along two profiles covering a region of 8 km x 8 km.
The tilt of the geophone inside the S-OBS influences the sensor characteristics. Since the orientation and tilt at the ocean bottom was unknown, approximately every 24 hours a calibration signal (a sequence of step-functions) was applied to the sensors of the ocean stations. This might be used to recover the actual sensor characteristics (eigenfrequency and damping).
The dataset contains 1) a info-folder with a) a README file; b) a file containing the times when calibration signals occurred (format: recorder_ID - date - time); c) the station table (ASCII; recorder_ID - latitude - longitude - (water)depth); d) a map of the region with the locations of the stations; 2) raw CUBE-formatted data; 3) converted mini-seed-formatted data (hourly files).
The Geophysical Instrument Pool Potsdam (GIPP) provides field instruments for (temporary) seismological studies (both controlled source and earthquake seismology) and for magnetotelluric (electromagnetic) experiments. The GIPP is operated by the GFZ Helmholtz Centre for Geosciences. The instrument facility is open for academic use. Instrument applications are evaluated and ranked by an external steering board. See Haberland and Ritter (2016) and https://www.gfz.de/gipp for more information.
Study area
130.018
71.5717
Geophysical Instrument Pool Potsdam
GIPP201315
Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ
http://doi.org/10.13039/501100010956