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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2023
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Online Access: | http://dx.doi.org/10.22541/essoar.170197105.58777865/v1 |
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crwinnower:10.22541/essoar.170197105.58777865/v1 2024-06-02T08:11:29+00:00 Seasonal tracer subduction in the Subpolar North Atlantic driven by submesoscale fronts Picard, Théo Gula, Jonathan Vic, Clement Mémery, Laurent 2023 http://dx.doi.org/10.22541/essoar.170197105.58777865/v1 unknown Authorea, Inc. posted-content 2023 crwinnower https://doi.org/10.22541/essoar.170197105.58777865/v1 2024-05-07T14:19:27Z 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. Other/Unknown Material North Atlantic The Winnower |
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language |
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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 |
Other/Unknown Material |
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 |
http://dx.doi.org/10.22541/essoar.170197105.58777865/v1 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_doi |
https://doi.org/10.22541/essoar.170197105.58777865/v1 |
_version_ |
1800757640467316736 |