Recent advances in the study of Arctic submarine permafrost

Submarine permafrost is perennially cryotic earth material that lies offshore. Most submarine permafrost is relict terrestrial permafrost beneath the Arctic shelf seas, was inundated after the last glaciation, and has been warming and thawing ever since. As a reservoir and confining layer for gas hy...

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Bibliographic Details
Main Authors: Angelopoulos, Michael, Overduin, Pier P., Miesner, Frederieke, Grigoriev, Mikhail N., Vasiliev, Alexander A.
Format: Text
Language:English
Published: FID GEO 2020
Subjects:
Arctic
Arctic Ocean
East Siberian Shelf
Climate change
Ice
permafrost
Sea ice
Online Access:https://dx.doi.org/10.23689/fidgeo-4439
https://e-docs.geo-leo.de/handle/11858/8785

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