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...

Full description

Bibliographic Details
Published in:Permafrost and Periglacial Processes
Main Authors: Morgenstern, Anne, Overduin, Pier Paul, Günther, Frank, Stettner, Samuel, Ramage, Justine, Schirrmeister, Lutz, Grigoriev, Mikhail N., Grosse, Guido, 1 Department of Permafrost Research Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research Potsdam Germany, 6 Melnikov Permafrost Institute, Siberian Branch Russian Academy of Sciences Yakutsk Russia
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.1002/ppp.2087
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8423