Marine electrical resistivity profile 3, Bykovsky Peninsula, Siberia

The data was collected with an IRIS Syscal Pro Deep Marine resistivity system that was equipped with a GPS and an echo-sounder to record water depths. The geoelectric cable had an electrode separation of 10 m and the electrodes were arranged in a reciprocal Wenner Schlumberger array. The offset betw...

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Bibliographic Details
Main Authors: Angelopoulos, Michael, Overduin, Pier Paul, Jenrich, Maren, Nitze, Ingmar, Günther, Frank, Strauss, Jens, Westermann, Sebastian, Schirrmeister, Lutz, Kholodov, Alexander L, Krautblatter, Michael, Grigoriev, Mikhail N, Grosse, Guido
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
Alas
AWI Arctic Land Expedition
BYK_profile3_parallel_to_shore
Bykovsky
CATS
CATS - The Changing Arctic Transpolar System
DEPTH
water
electrical resistivity
Electrical resistivity tomography
ERT
LATITUDE
Lena2017
Lena Delta
LONGITUDE
Near surface geophysics
NUNATARYUK
Permafrost thaw and the changing Arctic coast
science for socioeconomic adaptation
PETA-CARB
POINT DISTANCE from start
Position
Rapid Permafrost Thaw in a Warming Arctic and Impacts on the Soil Organic Carbon Pool
Resistivity
apparent
Resistivity profiler
IRIS Syscal Pro Deep Marine
RU-Land_2017_Lena
Submarine Permafrost
subsea permafrost
talik
Thermokarst Lagoon
Arctic
Peta
Talik
lena delta
permafrost
Thermokarst
Siberia
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.934163
https://doi.org/10.1594/PANGAEA.934163
Description
Summary:The data was collected with an IRIS Syscal Pro Deep Marine resistivity system that was equipped with a GPS and an echo-sounder to record water depths. The geoelectric cable had an electrode separation of 10 m and the electrodes were arranged in a reciprocal Wenner Schlumberger array. The offset between the first electrode and the boat was approximately 10 m.

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