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The Cryosphere An interactive open-access journal of the European Geosciences Union
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TC | Volume 12, issue 9
The Cryosphere, 12, 3001–3015, 2018
https://doi.org/10.5194/tc-12-3001-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 12, 3001–3015, 2018
https://doi.org/10.5194/tc-12-3001-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 21 Sep 2018

Research article | 21 Sep 2018

Modelling the late Holocene and future evolution of Monacobreen, northern Spitsbergen

Johannes Oerlemans
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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
AR by Johannes Oerlemans on behalf of the Authors (26 Jun 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (27 Jun 2018) by Valentina Radic
RR by Anonymous Referee #1 (07 Jul 2018)
ED: Reconsider after major revisions (09 Jul 2018) by Valentina Radic
AR by Lorena Grabowski on behalf of the Authors (31 Jul 2018)  Author's response
ED: Publish subject to minor revisions (review by editor) (10 Aug 2018) by Valentina Radic
AR by Johannes Oerlemans on behalf of the Authors (15 Aug 2018)  Author's response    Manuscript
ED: Publish as is (26 Aug 2018) by Valentina Radic
Publications Copernicus
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Short summary
Monacobreen is a 40 km long surge-type tidewater glacier in northern Spitsbergen. The front is retreating fast. Calculations with a glacier model predict that due to future climate warming this glacier will have lost 20 to 40 % of its volume by the year 2100. Because of the glacier's memory, much of the response will come after 2100, even if the climatic conditions would stabilize.
Monacobreen is a 40 km long surge-type tidewater glacier in northern Spitsbergen. The front is...
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