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Climate of the Past An interactive open-access journal of the European Geosciences Union
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CP | Articles | Volume 16, issue 4
Clim. Past, 16, 1127–1143, 2020
https://doi.org/10.5194/cp-16-1127-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Clim. Past, 16, 1127–1143, 2020
https://doi.org/10.5194/cp-16-1127-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

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 et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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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
Publications Copernicus
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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.
The Labrador Sea is important for the modern global thermohaline circulation system through the...
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