Articles | Volume 13, issue 12
Clim. Past, 13, 1717–1749, 2017
Clim. Past, 13, 1717–1749, 2017

Research article 30 Nov 2017

Research article | 30 Nov 2017

Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation

Martin Bartels et al.


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
ED: Publish subject to minor revisions (review by Editor) (15 Jul 2017) by Arne Winguth
AR by Martin Bartels on behalf of the Authors (15 Sep 2017)  Author's response    Manuscript
ED: Publish as is (16 Oct 2017) by Arne Winguth
Short summary
Multi-proxy analyses (i.a., benthic foraminiferal assemblages and sedimentary properties) of a marine record from Woodfjorden at the northern Svalbard margin (Norwegian Arctic) illustrate a significant contribution of relatively warm Atlantic water to the destabilization of tidewater glaciers, especially during the deglaciation and early Holocene (until ~ 7800 years ago), whereas its influence on glacier activity has been fading during the last 2 millennia, enabling glacier readvances.