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...
Published in: | Permafrost and Periglacial Processes |
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Main Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2020
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Subjects: | |
Online Access: | https://doi.org/10.1002/ppp.2087 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8423 |