From interannual to decadal: 17 years of boundary current transports at the exit of the Labrador Sea

Over the past 17 years, the western boundary current system of the Labrador Sea has been closely observed by maintaining the 53°N observatory (moorings and shipboard station data) measuring the top-to-bottom flow field offshore from the Labrador shelf break. Volume transports for the North Atlantic...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Zantopp, Rainer J., Fischer, Jürgen, Visbeck, Martin, Karstensen, Johannes
Format: Article in Journal/Newspaper
Language:English
Published: AGU (American Geophysical Union) 2017
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/37383/
https://oceanrep.geomar.de/id/eprint/37383/1/jgrc22144.pdf
https://doi.org/10.1002/2016JC012271
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spelling ftoceanrep:oai:oceanrep.geomar.de:37383 2023-05-15T17:06:01+02:00 From interannual to decadal: 17 years of boundary current transports at the exit of the Labrador Sea Zantopp, Rainer J. Fischer, Jürgen Visbeck, Martin Karstensen, Johannes 2017-03-04 text https://oceanrep.geomar.de/id/eprint/37383/ https://oceanrep.geomar.de/id/eprint/37383/1/jgrc22144.pdf https://doi.org/10.1002/2016JC012271 en eng AGU (American Geophysical Union) Wiley https://oceanrep.geomar.de/id/eprint/37383/1/jgrc22144.pdf Zantopp, R. J. , Fischer, J. , Visbeck, M. and Karstensen, J. (2017) From interannual to decadal: 17 years of boundary current transports at the exit of the Labrador Sea. Open Access Journal of Geophysical Research: Oceans, 122 (3). pp. 1724-1748. DOI 10.1002/2016JC012271 <https://doi.org/10.1002/2016JC012271>. doi:10.1002/2016JC012271 cc_by_4.0 info:eu-repo/semantics/openAccess Article PeerReviewed info:eu-repo/semantics/article 2017 ftoceanrep https://doi.org/10.1002/2016JC012271 2023-04-07T15:32:19Z Over the past 17 years, the western boundary current system of the Labrador Sea has been closely observed by maintaining the 53°N observatory (moorings and shipboard station data) measuring the top-to-bottom flow field offshore from the Labrador shelf break. Volume transports for the North Atlantic Deep Water (NADW) components were calculated using different methods, including gap filling procedures for deployment periods with suboptimal instrument coverage. On average the Deep Western Boundary Current (DWBC) carries 30.2 ± 6.6 Sv of NADW southward, which are almost equally partitioned between Labrador Sea Water (LSW, 14.9 ± 3.9 Sv) and Lower North Atlantic Deep Water (LNADW, 15.3 ± 3.8 Sv). The transport variability ranges from days to decades, with the most prominent multiyear fluctuations at interannual to near decadal time scales (±5 Sv) in the LNADW overflow water mass. These long-term fluctuations appear to be in phase with the NAO-modulated wind fluctuations. The boundary current system off Labrador occurs as a conglomerate of nearly independent components, namely, the shallow Labrador Current, the weakly sheared LSW range, and the deep baroclinic, bottom-intensified current core of the LNADW, all of which are part of the cyclonic Labrador Sea circulation. This structure is relatively stable over time, and the 120 km wide boundary current is constrained seaward by a weak counterflow which reduces the deep water export by 10–15%. Article in Journal/Newspaper Labrador Sea NADW North Atlantic Deep Water North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Labrador Shelf ENVELOPE(-58.000,-58.000,56.000,56.000) Journal of Geophysical Research: Oceans 122 3 1724 1748
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description Over the past 17 years, the western boundary current system of the Labrador Sea has been closely observed by maintaining the 53°N observatory (moorings and shipboard station data) measuring the top-to-bottom flow field offshore from the Labrador shelf break. Volume transports for the North Atlantic Deep Water (NADW) components were calculated using different methods, including gap filling procedures for deployment periods with suboptimal instrument coverage. On average the Deep Western Boundary Current (DWBC) carries 30.2 ± 6.6 Sv of NADW southward, which are almost equally partitioned between Labrador Sea Water (LSW, 14.9 ± 3.9 Sv) and Lower North Atlantic Deep Water (LNADW, 15.3 ± 3.8 Sv). The transport variability ranges from days to decades, with the most prominent multiyear fluctuations at interannual to near decadal time scales (±5 Sv) in the LNADW overflow water mass. These long-term fluctuations appear to be in phase with the NAO-modulated wind fluctuations. The boundary current system off Labrador occurs as a conglomerate of nearly independent components, namely, the shallow Labrador Current, the weakly sheared LSW range, and the deep baroclinic, bottom-intensified current core of the LNADW, all of which are part of the cyclonic Labrador Sea circulation. This structure is relatively stable over time, and the 120 km wide boundary current is constrained seaward by a weak counterflow which reduces the deep water export by 10–15%.
format Article in Journal/Newspaper
author Zantopp, Rainer J.
Fischer, Jürgen
Visbeck, Martin
Karstensen, Johannes
spellingShingle Zantopp, Rainer J.
Fischer, Jürgen
Visbeck, Martin
Karstensen, Johannes
From interannual to decadal: 17 years of boundary current transports at the exit of the Labrador Sea
author_facet Zantopp, Rainer J.
Fischer, Jürgen
Visbeck, Martin
Karstensen, Johannes
author_sort Zantopp, Rainer J.
title From interannual to decadal: 17 years of boundary current transports at the exit of the Labrador Sea
title_short From interannual to decadal: 17 years of boundary current transports at the exit of the Labrador Sea
title_full From interannual to decadal: 17 years of boundary current transports at the exit of the Labrador Sea
title_fullStr From interannual to decadal: 17 years of boundary current transports at the exit of the Labrador Sea
title_full_unstemmed From interannual to decadal: 17 years of boundary current transports at the exit of the Labrador Sea
title_sort from interannual to decadal: 17 years of boundary current transports at the exit of the labrador sea
publisher AGU (American Geophysical Union)
publishDate 2017
url https://oceanrep.geomar.de/id/eprint/37383/
https://oceanrep.geomar.de/id/eprint/37383/1/jgrc22144.pdf
https://doi.org/10.1002/2016JC012271
long_lat ENVELOPE(-58.000,-58.000,56.000,56.000)
geographic Labrador Shelf
geographic_facet Labrador Shelf
genre Labrador Sea
NADW
North Atlantic Deep Water
North Atlantic
genre_facet Labrador Sea
NADW
North Atlantic Deep Water
North Atlantic
op_relation https://oceanrep.geomar.de/id/eprint/37383/1/jgrc22144.pdf
Zantopp, R. J. , Fischer, J. , Visbeck, M. and Karstensen, J. (2017) From interannual to decadal: 17 years of boundary current transports at the exit of the Labrador Sea. Open Access Journal of Geophysical Research: Oceans, 122 (3). pp. 1724-1748. DOI 10.1002/2016JC012271 <https://doi.org/10.1002/2016JC012271>.
doi:10.1002/2016JC012271
op_rights cc_by_4.0
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1002/2016JC012271
container_title Journal of Geophysical Research: Oceans
container_volume 122
container_issue 3
container_start_page 1724
op_container_end_page 1748
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