Articles | Volume 16, issue 4
https://doi.org/10.5194/cp-16-1127-2020
https://doi.org/10.5194/cp-16-1127-2020
Research article
 | 
03 Jul 2020
Research article |  | 03 Jul 2020

Surface and subsurface Labrador Shelf water mass conditions during the last 6000 years

Annalena A. Lochte, Ralph Schneider, Markus Kienast, Janne Repschläger, Thomas Blanz, Dieter Garbe-Schönberg, and Nils Andersen

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (21 Jan 2020) by Bjørg Risebrobakken
AR by Anna Wenzel on behalf of the Authors (23 Mar 2020)  Author's response    Manuscript
ED: Publish subject to technical corrections (24 Mar 2020) by Bjørg Risebrobakken
AR by Annalena Lochte on behalf of the Authors (03 May 2020)  Author's response    Manuscript
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Short summary
The Labrador Sea is important for the modern global thermohaline circulation system through the formation of Labrador Sea Water. However, the role of the southward flowing Labrador Current in Labrador Sea convection is still debated. In order to better assess its role in deep-water formation and climate variability, we present high-resolution mid- to late Holocene records of sea surface and bottom water temperatures, freshening, and sea ice cover on the Labrador Shelf during the last 6000 years.