Mesoscale Eddies in the Arctic Ocean: Insights from a High-Resolution Simulation

Mesoscale eddies are significant drivers of the dynamics in the Arctic Ocean and are crucial to understanding ongoing changes in the region. However, adequately resolving these small-scale features in ocean models is challenging, and high-resolution simulations are required to accurately represent m...

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Main Authors: Müller, V., Qang, Q., Koldunov, N., Sergey, D., Thomas, J.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020474
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5020474 2023-07-30T04:00:44+02:00 Mesoscale Eddies in the Arctic Ocean: Insights from a High-Resolution Simulation Müller, V. Qang, Q. Koldunov, N. Sergey, D. Thomas, J. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020474 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-3184 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020474 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-3184 2023-07-09T23:40:17Z Mesoscale eddies are significant drivers of the dynamics in the Arctic Ocean and are crucial to understanding ongoing changes in the region. However, adequately resolving these small-scale features in ocean models is challenging, and high-resolution simulations are required to accurately represent mesoscale processes.In this study, we utilized a simulation from the unstructured-mesh Finite volumE Sea ice-Ocean Model (FESOM2) with a 1-km horizontal resolution in the Arctic Ocean, which can be considered eddy-resolving. This model has been previously used to study the distribution of eddy kinetic energy (EKE) in the Arctic, and we now evaluate the changes of EKE in the Eurasian Basin from seasonal to interannual time scales and their connection to other properties, such as sea-ice cover, baroclinic conversion rate, and stratification.We found that EKE seasonality is predominantly influenced by changes in sea-ice cover, while monthly anomalies have different drivers at different depths. The mixed layer, which is strongly linked to the surface, is primarily affected by sea-ice variability. In contrast, deeper levels are shielded from the surface by stratification and are more strongly influenced by baroclinic conversion.Overall, our high-resolution simulation sheds light on the complex relationship between mesoscale eddies, sea-ice cover, baroclinic conversion and stratification in the Arctic Ocean. Conference Object Arctic Arctic Ocean Sea ice GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic Arctic Ocean
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Mesoscale eddies are significant drivers of the dynamics in the Arctic Ocean and are crucial to understanding ongoing changes in the region. However, adequately resolving these small-scale features in ocean models is challenging, and high-resolution simulations are required to accurately represent mesoscale processes.In this study, we utilized a simulation from the unstructured-mesh Finite volumE Sea ice-Ocean Model (FESOM2) with a 1-km horizontal resolution in the Arctic Ocean, which can be considered eddy-resolving. This model has been previously used to study the distribution of eddy kinetic energy (EKE) in the Arctic, and we now evaluate the changes of EKE in the Eurasian Basin from seasonal to interannual time scales and their connection to other properties, such as sea-ice cover, baroclinic conversion rate, and stratification.We found that EKE seasonality is predominantly influenced by changes in sea-ice cover, while monthly anomalies have different drivers at different depths. The mixed layer, which is strongly linked to the surface, is primarily affected by sea-ice variability. In contrast, deeper levels are shielded from the surface by stratification and are more strongly influenced by baroclinic conversion.Overall, our high-resolution simulation sheds light on the complex relationship between mesoscale eddies, sea-ice cover, baroclinic conversion and stratification in the Arctic Ocean.
format Conference Object
author Müller, V.
Qang, Q.
Koldunov, N.
Sergey, D.
Thomas, J.
spellingShingle Müller, V.
Qang, Q.
Koldunov, N.
Sergey, D.
Thomas, J.
Mesoscale Eddies in the Arctic Ocean: Insights from a High-Resolution Simulation
author_facet Müller, V.
Qang, Q.
Koldunov, N.
Sergey, D.
Thomas, J.
author_sort Müller, V.
title Mesoscale Eddies in the Arctic Ocean: Insights from a High-Resolution Simulation
title_short Mesoscale Eddies in the Arctic Ocean: Insights from a High-Resolution Simulation
title_full Mesoscale Eddies in the Arctic Ocean: Insights from a High-Resolution Simulation
title_fullStr Mesoscale Eddies in the Arctic Ocean: Insights from a High-Resolution Simulation
title_full_unstemmed Mesoscale Eddies in the Arctic Ocean: Insights from a High-Resolution Simulation
title_sort mesoscale eddies in the arctic ocean: insights from a high-resolution simulation
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020474
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-3184
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020474
op_doi https://doi.org/10.57757/IUGG23-3184
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