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...
Main Authors: | , , , , , , , |
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Format: | Text |
Language: | English |
Published: |
FID GEO
2020
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Subjects: | |
Online Access: | https://dx.doi.org/10.23689/fidgeo-4083 https://e-docs.geo-leo.de/handle/11858/8423 |