Articles | Volume 11, issue 11
Clim. Past, 11, 1507–1525, 2015
Clim. Past, 11, 1507–1525, 2015

Research article 12 Nov 2015

Research article | 12 Nov 2015

Stratification of surface waters during the last glacial millennial climatic events: a key factor in subsurface and deep-water mass dynamics

M. Wary 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: Reconsider after major revisions (02 Aug 2015) by Volker Rath
AR by Mélanie Wary on behalf of the Authors (19 Aug 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (19 Aug 2015) by Volker Rath
RR by Anonymous Referee #2 (14 Sep 2015)
ED: Publish as is (18 Oct 2015) by Volker Rath
Short summary
This study reports the hydrological variations recorded at different depths of the water column SW of the Faeroe Is. during the last glacial abrupt climatic events (Heinrich events and Dansgaard-Oeschger cycles). Our combined multiproxy and high-resolution approach allows us to evidence that 1) Greenland and Heinrich stadials were characterized by strong stratification of surface waters, 2) this surface stratification seems to have played a key role in the dynamics of the underlying water masses