Predictive ability of a linear theoretical model for the time-varying circulation in the Nordic seas and Arctic Ocean

In this study, we re-examine the use of an existing theoretical model for predicting the time-variable large-scale circulation along contours of constant ambient potential vorticity, given by f/H, in the Nordic Seas and Arctic Ocean. The theoretical model is an integral relation derived from the lin...

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Main Authors: Sjur, A., Isachsen, P., Nilsson, J., Ryseth, M., Lacasce, J.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017839
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5017839 2023-08-27T04:07:40+02:00 Predictive ability of a linear theoretical model for the time-varying circulation in the Nordic seas and Arctic Ocean Sjur, A. Isachsen, P. Nilsson, J. Ryseth, M. Lacasce, J. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017839 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1752 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017839 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-1752 2023-08-06T23:41:22Z In this study, we re-examine the use of an existing theoretical model for predicting the time-variable large-scale circulation along contours of constant ambient potential vorticity, given by f/H, in the Nordic Seas and Arctic Ocean. The theoretical model is an integral relation derived from the linear depth-averaged shallow water equations, and assumes that the circulation is driven by surface stresses and regulated by bottom drag. By applying this simplified model to a high-resolution numerical simulation, we assess its ability to accurately predict the circulation. Improvements from earlier examinations include better parametrization of stresses in ice-covered regions and higher resolution in the numerical simulation. Our results show that the linear model agrees well with the complex model. This indicates that much of the variability in the large-scale circulation can be explained by linear processes. However, we find that the performance of the linear model depends on the direction of the circulation, with the linear model overestimating anti-cyclonic circulation. This suggests that additional processes, not captured in the linear model, play a crucial role in anti-cyclonic circulation. Conference Object Arctic Arctic Ocean Nordic Seas 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 In this study, we re-examine the use of an existing theoretical model for predicting the time-variable large-scale circulation along contours of constant ambient potential vorticity, given by f/H, in the Nordic Seas and Arctic Ocean. The theoretical model is an integral relation derived from the linear depth-averaged shallow water equations, and assumes that the circulation is driven by surface stresses and regulated by bottom drag. By applying this simplified model to a high-resolution numerical simulation, we assess its ability to accurately predict the circulation. Improvements from earlier examinations include better parametrization of stresses in ice-covered regions and higher resolution in the numerical simulation. Our results show that the linear model agrees well with the complex model. This indicates that much of the variability in the large-scale circulation can be explained by linear processes. However, we find that the performance of the linear model depends on the direction of the circulation, with the linear model overestimating anti-cyclonic circulation. This suggests that additional processes, not captured in the linear model, play a crucial role in anti-cyclonic circulation.
format Conference Object
author Sjur, A.
Isachsen, P.
Nilsson, J.
Ryseth, M.
Lacasce, J.
spellingShingle Sjur, A.
Isachsen, P.
Nilsson, J.
Ryseth, M.
Lacasce, J.
Predictive ability of a linear theoretical model for the time-varying circulation in the Nordic seas and Arctic Ocean
author_facet Sjur, A.
Isachsen, P.
Nilsson, J.
Ryseth, M.
Lacasce, J.
author_sort Sjur, A.
title Predictive ability of a linear theoretical model for the time-varying circulation in the Nordic seas and Arctic Ocean
title_short Predictive ability of a linear theoretical model for the time-varying circulation in the Nordic seas and Arctic Ocean
title_full Predictive ability of a linear theoretical model for the time-varying circulation in the Nordic seas and Arctic Ocean
title_fullStr Predictive ability of a linear theoretical model for the time-varying circulation in the Nordic seas and Arctic Ocean
title_full_unstemmed Predictive ability of a linear theoretical model for the time-varying circulation in the Nordic seas and Arctic Ocean
title_sort predictive ability of a linear theoretical model for the time-varying circulation in the nordic seas and arctic ocean
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017839
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Nordic Seas
genre_facet Arctic
Arctic Ocean
Nordic Seas
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1752
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017839
op_doi https://doi.org/10.57757/IUGG23-1752
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