The interior spreading story of Labrador Sea Water

The unique convective anomalies of Labrador Sea Water (LSW) can be used as advective tracers when assessing equatorward spreading pathways and timescales of LSW. In this study, we explore advective pathways of two LSW classes formed in the 1990s and early 2000s, respectively, along constant neutral...

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Published in:Frontiers in Marine Science
Main Authors: Chomiak, Leah, Volkov, Denis, Schmid, Claudia
Format: Article in Journal/Newspaper
Language:unknown
Published: Frontiers Media SA 2023
Subjects:
Online Access:http://dx.doi.org/10.3389/fmars.2023.1270463
https://www.frontiersin.org/articles/10.3389/fmars.2023.1270463/full
id crfrontiers:10.3389/fmars.2023.1270463
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spelling crfrontiers:10.3389/fmars.2023.1270463 2024-02-11T10:05:36+01:00 The interior spreading story of Labrador Sea Water Chomiak, Leah Volkov, Denis Schmid, Claudia 2023 http://dx.doi.org/10.3389/fmars.2023.1270463 https://www.frontiersin.org/articles/10.3389/fmars.2023.1270463/full unknown Frontiers Media SA https://creativecommons.org/licenses/by/4.0/ Frontiers in Marine Science volume 10 ISSN 2296-7745 Ocean Engineering Water Science and Technology Aquatic Science Global and Planetary Change Oceanography journal-article 2023 crfrontiers https://doi.org/10.3389/fmars.2023.1270463 2024-01-26T10:07:56Z The unique convective anomalies of Labrador Sea Water (LSW) can be used as advective tracers when assessing equatorward spreading pathways and timescales of LSW. In this study, we explore advective pathways of two LSW classes formed in the 1990s and early 2000s, respectively, along constant neutral density planes. Hydrographic observations showcase the prevalence of both LSW classes within the Atlantic interior, supporting a recirculation feature that branches from the Deep Western Boundary Current (DWBC) at 36°N among other pathways. Spreading characteristics of both LSW classes from the Labrador Sea to the subtropics are reinforced through a spatial pattern analysis of salinity anomalies and geostrophic velocities along the characteristic neutral density planes of each respective LSW class. We observe both classes to advect out of the Labrador Sea to (i) the eastern subpolar region and down the eastern boundary towards the Atlantic interior, (ii) directly into the Atlantic interior likely from an injection by recirculations from the subpolar gyre and DWBC leakage, and (iii) equatorward along the western boundary via the DWBC. Findings highlight the abundance of LSW within the Atlantic interior, not just along the western boundary, suggesting that interior pathways play an influential role on the export of these subpolar climate signals. Article in Journal/Newspaper Labrador Sea Frontiers (Publisher) Frontiers in Marine Science 10
institution Open Polar
collection Frontiers (Publisher)
op_collection_id crfrontiers
language unknown
topic Ocean Engineering
Water Science and Technology
Aquatic Science
Global and Planetary Change
Oceanography
spellingShingle Ocean Engineering
Water Science and Technology
Aquatic Science
Global and Planetary Change
Oceanography
Chomiak, Leah
Volkov, Denis
Schmid, Claudia
The interior spreading story of Labrador Sea Water
topic_facet Ocean Engineering
Water Science and Technology
Aquatic Science
Global and Planetary Change
Oceanography
description The unique convective anomalies of Labrador Sea Water (LSW) can be used as advective tracers when assessing equatorward spreading pathways and timescales of LSW. In this study, we explore advective pathways of two LSW classes formed in the 1990s and early 2000s, respectively, along constant neutral density planes. Hydrographic observations showcase the prevalence of both LSW classes within the Atlantic interior, supporting a recirculation feature that branches from the Deep Western Boundary Current (DWBC) at 36°N among other pathways. Spreading characteristics of both LSW classes from the Labrador Sea to the subtropics are reinforced through a spatial pattern analysis of salinity anomalies and geostrophic velocities along the characteristic neutral density planes of each respective LSW class. We observe both classes to advect out of the Labrador Sea to (i) the eastern subpolar region and down the eastern boundary towards the Atlantic interior, (ii) directly into the Atlantic interior likely from an injection by recirculations from the subpolar gyre and DWBC leakage, and (iii) equatorward along the western boundary via the DWBC. Findings highlight the abundance of LSW within the Atlantic interior, not just along the western boundary, suggesting that interior pathways play an influential role on the export of these subpolar climate signals.
format Article in Journal/Newspaper
author Chomiak, Leah
Volkov, Denis
Schmid, Claudia
author_facet Chomiak, Leah
Volkov, Denis
Schmid, Claudia
author_sort Chomiak, Leah
title The interior spreading story of Labrador Sea Water
title_short The interior spreading story of Labrador Sea Water
title_full The interior spreading story of Labrador Sea Water
title_fullStr The interior spreading story of Labrador Sea Water
title_full_unstemmed The interior spreading story of Labrador Sea Water
title_sort interior spreading story of labrador sea water
publisher Frontiers Media SA
publishDate 2023
url http://dx.doi.org/10.3389/fmars.2023.1270463
https://www.frontiersin.org/articles/10.3389/fmars.2023.1270463/full
genre Labrador Sea
genre_facet Labrador Sea
op_source Frontiers in Marine Science
volume 10
ISSN 2296-7745
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3389/fmars.2023.1270463
container_title Frontiers in Marine Science
container_volume 10
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