Seasonal tracer subduction in the Subpolar North Atlantic driven by submesoscale fronts

Submesoscale flows (0.1 - 10 km) are often associated with large vertical velocities, which can have a significant impact on the transport of surface tracers, such as carbon. However, global models do not adequately account for these small-scale effects, which still require a proper parameterization...

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Main Authors: Picard, Théo, Gula, Jonathan, Vic, Clement, Mémery, Laurent
Format: Article in Journal/Newspaper
Language:English
Published: Authorea, Inc. 2023
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00867/97911/107009.pdf
https://doi.org/10.22541/essoar.170197105.58777865/v1
https://archimer.ifremer.fr/doc/00867/97911/
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spelling ftarchimer:oai:archimer.ifremer.fr:97911 2024-01-14T10:09:05+01:00 Seasonal tracer subduction in the Subpolar North Atlantic driven by submesoscale fronts Picard, Théo Gula, Jonathan Vic, Clement Mémery, Laurent 2023-12-07 application/pdf https://archimer.ifremer.fr/doc/00867/97911/107009.pdf https://doi.org/10.22541/essoar.170197105.58777865/v1 https://archimer.ifremer.fr/doc/00867/97911/ eng eng Authorea, Inc. https://archimer.ifremer.fr/doc/00867/97911/107009.pdf doi:10.22541/essoar.170197105.58777865/v1 https://archimer.ifremer.fr/doc/00867/97911/ info:eu-repo/semantics/openAccess restricted use ESS Open Archive . (Authorea, Inc.) In Press text Article info:eu-repo/semantics/article 2023 ftarchimer https://doi.org/10.22541/essoar.170197105.58777865/v1 2023-12-19T23:51:09Z Submesoscale flows (0.1 - 10 km) are often associated with large vertical velocities, which can have a significant impact on the transport of surface tracers, such as carbon. However, global models do not adequately account for these small-scale effects, which still require a proper parameterization. In this study, we introduced a passive tracer into the mixed layer of the northern Atlantic Ocean using a CROCO simulation with a high horizontal resolution of Δx = 800 m, aiming to investigate the seasonal submesoscale effects on vertical transport. Using surface vorticity and strain criteria, we identified regions with submesoscale fronts and quantified the associated subduction, that is the export of tracer below the mixed layer depth. The results suggest that the tracer vertical distribution and the contribution of frontal subduction can be estimated from surface strain and vorticity. Notably, we observed significant seasonal variations. In winter, the submesoscale fronts contribute up to 40% of the vertical advective transport of tracer below the mixed layer, while representing only 5% of the domain. Conversely, in summer, fronts account for less than 1% of the domain and do not contribute significantly to the transport below the mixed layer. The findings of this study contribute to a better understanding of the seasonal water subduction due to fronts in the region. Article in Journal/Newspaper North Atlantic Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer)
institution Open Polar
collection Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer)
op_collection_id ftarchimer
language English
description Submesoscale flows (0.1 - 10 km) are often associated with large vertical velocities, which can have a significant impact on the transport of surface tracers, such as carbon. However, global models do not adequately account for these small-scale effects, which still require a proper parameterization. In this study, we introduced a passive tracer into the mixed layer of the northern Atlantic Ocean using a CROCO simulation with a high horizontal resolution of Δx = 800 m, aiming to investigate the seasonal submesoscale effects on vertical transport. Using surface vorticity and strain criteria, we identified regions with submesoscale fronts and quantified the associated subduction, that is the export of tracer below the mixed layer depth. The results suggest that the tracer vertical distribution and the contribution of frontal subduction can be estimated from surface strain and vorticity. Notably, we observed significant seasonal variations. In winter, the submesoscale fronts contribute up to 40% of the vertical advective transport of tracer below the mixed layer, while representing only 5% of the domain. Conversely, in summer, fronts account for less than 1% of the domain and do not contribute significantly to the transport below the mixed layer. The findings of this study contribute to a better understanding of the seasonal water subduction due to fronts in the region.
format Article in Journal/Newspaper
author Picard, Théo
Gula, Jonathan
Vic, Clement
Mémery, Laurent
spellingShingle Picard, Théo
Gula, Jonathan
Vic, Clement
Mémery, Laurent
Seasonal tracer subduction in the Subpolar North Atlantic driven by submesoscale fronts
author_facet Picard, Théo
Gula, Jonathan
Vic, Clement
Mémery, Laurent
author_sort Picard, Théo
title Seasonal tracer subduction in the Subpolar North Atlantic driven by submesoscale fronts
title_short Seasonal tracer subduction in the Subpolar North Atlantic driven by submesoscale fronts
title_full Seasonal tracer subduction in the Subpolar North Atlantic driven by submesoscale fronts
title_fullStr Seasonal tracer subduction in the Subpolar North Atlantic driven by submesoscale fronts
title_full_unstemmed Seasonal tracer subduction in the Subpolar North Atlantic driven by submesoscale fronts
title_sort seasonal tracer subduction in the subpolar north atlantic driven by submesoscale fronts
publisher Authorea, Inc.
publishDate 2023
url https://archimer.ifremer.fr/doc/00867/97911/107009.pdf
https://doi.org/10.22541/essoar.170197105.58777865/v1
https://archimer.ifremer.fr/doc/00867/97911/
genre North Atlantic
genre_facet North Atlantic
op_source ESS Open Archive . (Authorea, Inc.) In Press
op_relation https://archimer.ifremer.fr/doc/00867/97911/107009.pdf
doi:10.22541/essoar.170197105.58777865/v1
https://archimer.ifremer.fr/doc/00867/97911/
op_rights info:eu-repo/semantics/openAccess
restricted use
op_doi https://doi.org/10.22541/essoar.170197105.58777865/v1
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