Articles | Volume 14, issue 6
The Cryosphere, 14, 1857–1873, 2020
https://doi.org/10.5194/tc-14-1857-2020
The Cryosphere, 14, 1857–1873, 2020
https://doi.org/10.5194/tc-14-1857-2020

Research article 11 Jun 2020

Research article | 11 Jun 2020

The current state and 125 kyr history of permafrost on the Kara Sea shelf: modeling constraints

Anatoliy Gavrilov et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (27 Jan 2020) by Christian Hauck
AR by Maria Cherbunina on behalf of the Authors (07 Mar 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (10 Mar 2020) by Christian Hauck
RR by Anonymous Referee #1 (19 Mar 2020)
RR by Anonymous Referee #2 (31 Mar 2020)
ED: Publish subject to minor revisions (review by editor) (03 Apr 2020) by Christian Hauck
AR by Maria Cherbunina on behalf of the Authors (12 Apr 2020)  Author's response    Manuscript
ED: Publish subject to technical corrections (28 Apr 2020) by Christian Hauck
AR by Maria Cherbunina on behalf of the Authors (03 May 2020)  Author's response    Manuscript
Download
Short summary
The geocryological study of the Arctic shelf remains insufficient for economic activity. The article presents a study of its evolution by methods of math modeling of heat transfer in rocks. As a result, a model of the evolution and current state of the cryolithozone of the Kara shelf was created based on ideas about the history of its geocryological development over the past 125 kyr. The modeling results are correlated to the available field data and are presented as a geocryological map.