Age model, alkenones and stable isotopes of sediment core MSM45-31-1 (MSM45_431-1) ...
The Labrador Sea is important for the modern global thermohaline circulation system through the formation of intermediate Labrador Sea Water (LSW) that has been hypothesized to stabilize the modern mode of North Atlantic deep-water circulation. The rate of LSW formation is controlled by the amount o...
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ftdatacite:10.1594/pangaea.904693 2024-09-15T18:09:53+00:00 Age model, alkenones and stable isotopes of sediment core MSM45-31-1 (MSM45_431-1) ... Lochte, Annalena Antonia Schneider, Ralph R Kienast, Markus Repschläger, Janne Blanz, Thomas Garbe-Schönberg, Dieter Andersen, Nils 2019 application/zip https://dx.doi.org/10.1594/pangaea.904693 https://doi.pangaea.de/10.1594/PANGAEA.904693 en eng PANGAEA https://dx.doi.org/10.5194/cp-16-1127-2020 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Alkenones Labrador Sea Mg/Ca paleothermometry Stable isotopes Gravity corer MSM45 Maria S. Merian article Collection Supplementary Publication Series of Datasets 2019 ftdatacite https://doi.org/10.1594/pangaea.90469310.5194/cp-16-1127-2020 2024-07-03T13:15:54Z The Labrador Sea is important for the modern global thermohaline circulation system through the formation of intermediate Labrador Sea Water (LSW) that has been hypothesized to stabilize the modern mode of North Atlantic deep-water circulation. The rate of LSW formation is controlled by the amount of winter heat loss to the atmosphere, the expanse of freshwater in the convection region and the inflow of saline waters from the Atlantic. The Labrador Sea, today, receives freshwater through the East and West Greenland Currents (EGC, WGC) and the Labrador Current (LC). Several studies have suggested the WGC to be the main supplier of freshwater to the Labrador Sea, but the role of the southward flowing LC in Labrador Sea convection is still debated. At the same time, many paleoceanographic reconstructions from the Labrador Shelf focussed on late Deglacial to early Holocene meltwater run-off from the Laurentide Ice Sheet (LIS), whereas little information exists about LC variability since the final melting of the ... : Supplement to: Lochte, Annalena Antonia; Schneider, Ralph R; Kienast, Markus; Repschläger, Janne; Blanz, Thomas; Garbe-Schönberg, Dieter; Andersen, Nils (2020): Surface and subsurface Labrador Shelf water mass conditions during the last 6000 years. Climate of the Past, 16(4), 1127-1143 ... Article in Journal/Newspaper Greenland Ice Sheet Labrador Sea North Atlantic Deep Water North Atlantic DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Alkenones Labrador Sea Mg/Ca paleothermometry Stable isotopes Gravity corer MSM45 Maria S. Merian |
spellingShingle |
Alkenones Labrador Sea Mg/Ca paleothermometry Stable isotopes Gravity corer MSM45 Maria S. Merian Lochte, Annalena Antonia Schneider, Ralph R Kienast, Markus Repschläger, Janne Blanz, Thomas Garbe-Schönberg, Dieter Andersen, Nils Age model, alkenones and stable isotopes of sediment core MSM45-31-1 (MSM45_431-1) ... |
topic_facet |
Alkenones Labrador Sea Mg/Ca paleothermometry Stable isotopes Gravity corer MSM45 Maria S. Merian |
description |
The Labrador Sea is important for the modern global thermohaline circulation system through the formation of intermediate Labrador Sea Water (LSW) that has been hypothesized to stabilize the modern mode of North Atlantic deep-water circulation. The rate of LSW formation is controlled by the amount of winter heat loss to the atmosphere, the expanse of freshwater in the convection region and the inflow of saline waters from the Atlantic. The Labrador Sea, today, receives freshwater through the East and West Greenland Currents (EGC, WGC) and the Labrador Current (LC). Several studies have suggested the WGC to be the main supplier of freshwater to the Labrador Sea, but the role of the southward flowing LC in Labrador Sea convection is still debated. At the same time, many paleoceanographic reconstructions from the Labrador Shelf focussed on late Deglacial to early Holocene meltwater run-off from the Laurentide Ice Sheet (LIS), whereas little information exists about LC variability since the final melting of the ... : Supplement to: Lochte, Annalena Antonia; Schneider, Ralph R; Kienast, Markus; Repschläger, Janne; Blanz, Thomas; Garbe-Schönberg, Dieter; Andersen, Nils (2020): Surface and subsurface Labrador Shelf water mass conditions during the last 6000 years. Climate of the Past, 16(4), 1127-1143 ... |
format |
Article in Journal/Newspaper |
author |
Lochte, Annalena Antonia Schneider, Ralph R Kienast, Markus Repschläger, Janne Blanz, Thomas Garbe-Schönberg, Dieter Andersen, Nils |
author_facet |
Lochte, Annalena Antonia Schneider, Ralph R Kienast, Markus Repschläger, Janne Blanz, Thomas Garbe-Schönberg, Dieter Andersen, Nils |
author_sort |
Lochte, Annalena Antonia |
title |
Age model, alkenones and stable isotopes of sediment core MSM45-31-1 (MSM45_431-1) ... |
title_short |
Age model, alkenones and stable isotopes of sediment core MSM45-31-1 (MSM45_431-1) ... |
title_full |
Age model, alkenones and stable isotopes of sediment core MSM45-31-1 (MSM45_431-1) ... |
title_fullStr |
Age model, alkenones and stable isotopes of sediment core MSM45-31-1 (MSM45_431-1) ... |
title_full_unstemmed |
Age model, alkenones and stable isotopes of sediment core MSM45-31-1 (MSM45_431-1) ... |
title_sort |
age model, alkenones and stable isotopes of sediment core msm45-31-1 (msm45_431-1) ... |
publisher |
PANGAEA |
publishDate |
2019 |
url |
https://dx.doi.org/10.1594/pangaea.904693 https://doi.pangaea.de/10.1594/PANGAEA.904693 |
genre |
Greenland Ice Sheet Labrador Sea North Atlantic Deep Water North Atlantic |
genre_facet |
Greenland Ice Sheet Labrador Sea North Atlantic Deep Water North Atlantic |
op_relation |
https://dx.doi.org/10.5194/cp-16-1127-2020 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.90469310.5194/cp-16-1127-2020 |
_version_ |
1810447476076838912 |