Thermo-erosional valleys in Siberian ice-rich permafrost

Thermal erosion is a major mechanism of permafrost degradation, resulting in characteristic landforms. We inventory thermo-erosional valleys in ice-rich coastal lowlands adjacent to the Siberian Laptev Sea based on remote sensing, Geographic Information System (GIS), and field investigations for a f...

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Bibliographic Details
Published in:Permafrost and Periglacial Processes
Main Authors: Morgenstern, Anne, Overduin, Pier Paul, Günther, Frank (Dr.), Stettner, Samuel, Ramage, Justine, Schirrmeister, Lutz (Dr.), Grigoriev, Mikhail N., Grosse, Guido (Prof. Dr.)
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
ddc:550
Institut für Geowissenschaften
Buor-Khaya
Khaya
Laptev Sea
Ice
laptev
lena river
permafrost
Thermokarst
Online Access:https://publishup.uni-potsdam.de/frontdoor/index/index/docId/57787
https://doi.org/10.1002/ppp.2087

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