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Volume 14, issue 6 | Copyright
Clim. Past, 14, 709-724, 2018
https://doi.org/10.5194/cp-14-709-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 06 Jun 2018

Research article | 06 Jun 2018

Ground surface temperature reconstruction for the last 500 years obtained from permafrost temperatures observed in the SHARE STELVIO Borehole, Italian Alps

Mauro Guglielmin et al.
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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
ED: Reconsider after major revisions (25 Jul 2017) by Volker Rath
AR by Mauro Guglielmin on behalf of the Authors (15 Sep 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (13 Oct 2017) by Volker Rath
RR by Anonymous Referee #1 (04 Jan 2018)
ED: Reconsider after major revisions (04 Jan 2018) by Volker Rath
AR by Mauro Guglielmin on behalf of the Authors (12 Feb 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (26 Feb 2018) by Volker Rath
RR by Anonymous Referee #1 (01 May 2018)
ED: Publish subject to technical corrections (01 May 2018) by Volker Rath
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Short summary
The reconstruction of ground surface temperature for the last 500 years, obtained at the deepest mountain permafrost borehole of the world (Stelvio Pass, 3000 m a.s.l., Italian Alps), is presented here. The main difference with respect to MAAT reconstructions obtained through other proxy data for all of Europe relates to post Little Ice Age (LIA) events. Indeed at this site a stronger cooling of ca 1 °C between 1940 and 1989 and even a more abrupt warming between 1990 and 2011 was detected.
The reconstruction of ground surface temperature for the last 500 years, obtained at the deepest...
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