Articles | Volume 11, issue 1
https://doi.org/10.5194/tc-11-635-2017
https://doi.org/10.5194/tc-11-635-2017
Research article
 | 
28 Feb 2017
Research article |  | 28 Feb 2017

Soil moisture redistribution and its effect on inter-annual active layer temperature and thickness variations in a dry loess terrace in Adventdalen, Svalbard

Carina Schuh, Andrew Frampton, and Hanne Hvidtfeldt Christiansen

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Andrew Frampton on behalf of the Authors (25 Nov 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (30 Nov 2016) by Julia Boike
RR by Anonymous Referee #2 (18 Dec 2016)
RR by Anonymous Referee #1 (20 Dec 2016)
ED: Publish subject to minor revisions (Editor review) (22 Dec 2016) by Julia Boike
AR by Andrew Frampton on behalf of the Authors (05 Jan 2017)  Author's response    Manuscript
ED: Publish subject to technical corrections (18 Jan 2017) by Julia Boike
AR by Andrew Frampton on behalf of the Authors (23 Jan 2017)  Author's response    Manuscript
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Short summary
This study investigates how soil moisture retention characteristics impact ice and moisture redistribution, heat transport and active layer thickness under permafrost conditions. This is relevant for understanding how climate change interacts with permafrost, which is important because there is much stored carbon in permafrost, which may be released to the atmosphere as permafrost degrades and may then act to further enhance climate warming.