NEW PERMAFROST FEATURE – DEP CRATER IN CENTRAL YAMAL (WEST SIBERIA, RUSIA) AS A RESPONSE TO LOCAL CLIMATE FLUCTUATIONS

This paper is based on field data obtained during short visits to a newly formed permafrost feature in a form of relatively narrow, deep crater. Excluding impossible and improbable versions of the crater’s development, the authors conclude that it originated from warmerground temperatures and an inc...

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Bibliographic Details
Published in:GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
Main Authors: Marina O. Leibman, Alexander I. Kizyakov, Andrei V. Plekhanov, Irina D. Streletskaya
Format: Article in Journal/Newspaper
Language:English
Published: Lomonosov Moscow State University 2014
Subjects:
yamal crater
tabular ground ice
cryopegs
gas hydrates
climate fluctuations
cryolithozone
pingo
pockmarks
Geography (General)
G1-922
Ice
permafrost
Siberia
Online Access:https://doi.org/10.24057/2071-9388-2014-7-4-68-79
https://doaj.org/article/6f1b1c96aa8f41e6ae81f7c8ed943eb3
Description
Summary:This paper is based on field data obtained during short visits to a newly formed permafrost feature in a form of relatively narrow, deep crater. Excluding impossible and improbable versions of the crater’s development, the authors conclude that it originated from warmerground temperatures and an increase in unfrozen water content, leading to an increase in pressure from gas emissions from permafrost and ground ice. This conclusion is also supported by known processes in the palaeo-geography of Yamal lakes and recent studies of gas-hydrate behavior and subsea processes in gas-bearing provinces.

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