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: | unknown |
Published: |
Wiley-Blackwell
2021
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/53398/ https://epic.awi.de/id/eprint/53398/1/Morgenstern_et_al_2020_PPP.pdf https://doi.org/10.1002/ppp.2087 https://hdl.handle.net/10013/epic.881ee26a-ed60-4540-82f4-75a084e71e5f |