Articles | Volume 15, issue 7
The Cryosphere, 15, 3423–3442, 2021
https://doi.org/10.5194/tc-15-3423-2021
The Cryosphere, 15, 3423–3442, 2021
https://doi.org/10.5194/tc-15-3423-2021

Research article 22 Jul 2021

Research article | 22 Jul 2021

Lateral thermokarst patterns in permafrost peat plateaus in northern Norway

Léo C. P. Martin 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: Publish subject to revisions (further review by editor and referees) (25 Apr 2021) by Christian Hauck
AR by Léo Martin on behalf of the Authors (05 May 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (05 May 2021) by Christian Hauck
RR by Anonymous Referee #1 (12 May 2021)
RR by Anonymous Referee #2 (31 May 2021)
ED: Publish subject to technical corrections (08 Jun 2021) by Christian Hauck
AR by Léo Martin on behalf of the Authors (14 Jun 2021)  Author's response    Manuscript
Download
Short summary
It is important to understand how permafrost landscapes respond to climate changes because their thaw can contribute to global warming. We investigate how a common permafrost morphology degrades using both field observations of the surface elevation and numerical modeling. We show that numerical models accounting for topographic changes related to permafrost degradation can reproduce the observed changes in nature and help us understand how parameters such as snow influence this phenomenon.