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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 11, issue 3
The Cryosphere, 11, 1059–1073, 2017
https://doi.org/10.5194/tc-11-1059-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 11, 1059–1073, 2017
https://doi.org/10.5194/tc-11-1059-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 05 May 2017

Research article | 05 May 2017

Response of seasonal soil freeze depth to climate change across China

Xiaoqing Peng et al.
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Tingjun Zhang on behalf of the Authors (09 Mar 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (21 Mar 2017) by Andreas Kääb
RR by Elchin Jafarov (24 Mar 2017)
ED: Publish subject to technical corrections (03 Apr 2017) by Andreas Kääb
AR by Tingjun Zhang on behalf of the Authors (06 Apr 2017)  Author's response    Manuscript
Publications Copernicus
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Short summary
Previous research has paid significant attention to permafrost, e.g. active layer thickness, soil temperature, area extent, and associated degradation leading to other changes. However, less focus has been given to seasonally frozen ground and vast area extent. We combined data from more than 800 observation stations, as well as gridded data, to investigate soil freeze depth across China. The results indicate that soil freeze depth decreases with climate warming.
Previous research has paid significant attention to permafrost, e.g. active layer thickness,...
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