Decomposing Barotropic Transport Variability in a High-Resolution Model of the North Atlantic Ocean
A method using a linear shallow water model is presented for decomposing the temporal variability of the barotropic stream function in a high-resolution ocean model. The method is based on the vertically averaged momentum equations and is applied to the time series of annual mean stream function fro...
Published in: | Journal of Geophysical Research: Oceans |
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American Geophysical Union (AGU)
2020
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ftunivliverpool:oai:livrepository.liverpool.ac.uk:3136473 2023-05-15T17:29:21+02:00 Decomposing Barotropic Transport Variability in a High-Resolution Model of the North Atlantic Ocean Wang, Yuan Greatbatch, Richard J Claus, Martin Sheng, Jinyu 2020 http://livrepository.liverpool.ac.uk/3136473/ https://doi.org/10.1029/2019jc015516 en eng American Geophysical Union (AGU) Wang, Yuan, Greatbatch, Richard J, Claus, Martin and Sheng, Jinyu (2020) Decomposing Barotropic Transport Variability in a High-Resolution Model of the North Atlantic Ocean. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 125 (5). Article NonPeerReviewed 2020 ftunivliverpool https://doi.org/10.1029/2019jc015516 2023-01-20T00:09:03Z A method using a linear shallow water model is presented for decomposing the temporal variability of the barotropic stream function in a high-resolution ocean model. The method is based on the vertically averaged momentum equations and is applied to the time series of annual mean stream function from the model configuration VIKING20 for the northern North Atlantic. An important result is the role played by the nonlinear advection terms in VIKING20 for driving transport. The method is illustrated by examining how the Gulf Stream transport in the recirculation region responds to the winter North Atlantic Oscillation (NAO). While no statistically significant response is found in the year overlapping with the winter NAO index, there is a tendency for the Gulf Stream transport to increase as the NAO becomes more positive. This becomes significant in lead years 1 and 2 when the mean flow advection and eddy momentum flux contributions, associated with nonlinear momentum advection, dominate. Only after 2 years, does the potential energy term, associated with the density field, start to play a role and it is only after 5 years that the transport dependence on the NAO ceases to be significant. It is also shown that the potential energy contribution to the transport stream function has significant memory of up to 5 years in the Labrador and Irminger Seas. However, it is only around the northern rim of these seas that VIKING20 and the transport reconstruction exhibit similar memory. This is due to masking by the mean flow advection and eddy momentum flux contributions. Article in Journal/Newspaper North Atlantic North Atlantic oscillation The University of Liverpool Repository Journal of Geophysical Research: Oceans 125 5 |
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Open Polar |
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The University of Liverpool Repository |
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ftunivliverpool |
language |
English |
description |
A method using a linear shallow water model is presented for decomposing the temporal variability of the barotropic stream function in a high-resolution ocean model. The method is based on the vertically averaged momentum equations and is applied to the time series of annual mean stream function from the model configuration VIKING20 for the northern North Atlantic. An important result is the role played by the nonlinear advection terms in VIKING20 for driving transport. The method is illustrated by examining how the Gulf Stream transport in the recirculation region responds to the winter North Atlantic Oscillation (NAO). While no statistically significant response is found in the year overlapping with the winter NAO index, there is a tendency for the Gulf Stream transport to increase as the NAO becomes more positive. This becomes significant in lead years 1 and 2 when the mean flow advection and eddy momentum flux contributions, associated with nonlinear momentum advection, dominate. Only after 2 years, does the potential energy term, associated with the density field, start to play a role and it is only after 5 years that the transport dependence on the NAO ceases to be significant. It is also shown that the potential energy contribution to the transport stream function has significant memory of up to 5 years in the Labrador and Irminger Seas. However, it is only around the northern rim of these seas that VIKING20 and the transport reconstruction exhibit similar memory. This is due to masking by the mean flow advection and eddy momentum flux contributions. |
format |
Article in Journal/Newspaper |
author |
Wang, Yuan Greatbatch, Richard J Claus, Martin Sheng, Jinyu |
spellingShingle |
Wang, Yuan Greatbatch, Richard J Claus, Martin Sheng, Jinyu Decomposing Barotropic Transport Variability in a High-Resolution Model of the North Atlantic Ocean |
author_facet |
Wang, Yuan Greatbatch, Richard J Claus, Martin Sheng, Jinyu |
author_sort |
Wang, Yuan |
title |
Decomposing Barotropic Transport Variability in a High-Resolution Model of the North Atlantic Ocean |
title_short |
Decomposing Barotropic Transport Variability in a High-Resolution Model of the North Atlantic Ocean |
title_full |
Decomposing Barotropic Transport Variability in a High-Resolution Model of the North Atlantic Ocean |
title_fullStr |
Decomposing Barotropic Transport Variability in a High-Resolution Model of the North Atlantic Ocean |
title_full_unstemmed |
Decomposing Barotropic Transport Variability in a High-Resolution Model of the North Atlantic Ocean |
title_sort |
decomposing barotropic transport variability in a high-resolution model of the north atlantic ocean |
publisher |
American Geophysical Union (AGU) |
publishDate |
2020 |
url |
http://livrepository.liverpool.ac.uk/3136473/ https://doi.org/10.1029/2019jc015516 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
Wang, Yuan, Greatbatch, Richard J, Claus, Martin and Sheng, Jinyu (2020) Decomposing Barotropic Transport Variability in a High-Resolution Model of the North Atlantic Ocean. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 125 (5). |
op_doi |
https://doi.org/10.1029/2019jc015516 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
125 |
container_issue |
5 |
_version_ |
1766123251813056512 |