Articles | Volume 17, issue 11
https://doi.org/10.5194/tc-17-4601-2023
https://doi.org/10.5194/tc-17-4601-2023
Brief communication
 | 
03 Nov 2023
Brief communication |  | 03 Nov 2023

Brief communication: Alternation of thaw zones and deep permafrost in the cold climate conditions of the East Siberian Mountains, Suntar-Khayata Range

Robert Sysolyatin, Sergei Serikov, Anatoly Kirillin, Andrey Litovko, and Maxim Sivtsev

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-49', Lutz Schirrmeister, 18 Apr 2023
    • AC1: 'Reply on RC1', ROBERT SYSOLYATIN, 10 Jul 2023
  • RC2: 'Comment on egusphere-2023-49', Anonymous Referee #2, 13 Jun 2023
    • AC2: 'Reply on RC2', ROBERT SYSOLYATIN, 10 Jul 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (18 Jul 2023) by Christian Hauck
AR by ROBERT SYSOLYATIN on behalf of the Authors (21 Jul 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (21 Jul 2023) by Christian Hauck
RR by Lutz Schirrmeister (28 Aug 2023)
ED: Publish subject to revisions (further review by editor and referees) (01 Sep 2023) by Christian Hauck
AR by ROBERT SYSOLYATIN on behalf of the Authors (04 Sep 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (28 Sep 2023) by Christian Hauck
AR by ROBERT SYSOLYATIN on behalf of the Authors (29 Sep 2023)  Author's response   Manuscript 
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Short summary
Permafrost conditions of the East Siberian Mountains are poorly known because of the severe climate, extreme terrain, and farness and scarcity of data. The ground temperature regime plays a key role in mountainous regions, influencing the environment, slope stability, geomorphological processes and hydrological processes. We present the results of recent examinations of the permafrost thickness variations, temperature regime of thaw zones (taliks) and permafrost of the Suntar-Khayata Range.