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
Main Authors: Morgenstern, Anne, Overduin, Pier Paul, Günther, Frank, Stettner, Samuel, Ramage, Justine, Schirrmeister, Lutz, Grigoriev, Mikhail N., Grosse, Guido
Format: Text
Language:English
Published: FID GEO 2020
Subjects:
Ice
Online Access:https://dx.doi.org/10.23689/fidgeo-4083
https://e-docs.geo-leo.de/handle/11858/8423