The Faroe-Shetland Channel Jet: Structure, Variability, and Driving Mechanisms
The Faroe-Bank Channel (FBC) is a key gateway through which dense overflow water of the Nordic Seas supplies the lower limb of the Atlantic Meridional Overturning Circulation. Most recently, it was discovered that a deep jet through the Faroe-Shetland Channel carries the bulk of this overflow water,...
Published in: | Journal of Geophysical Research: Oceans |
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Online Access: | https://digitalcommons.uri.edu/gsofacpubs/2232 https://doi.org/10.1029/2022JC019083 |
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ftunivrhodeislan:oai:digitalcommons.uri.edu:gsofacpubs-3201 2024-02-11T10:05:59+01:00 The Faroe-Shetland Channel Jet: Structure, Variability, and Driving Mechanisms Chafik, L. Nilsson, J. Rossby, T. Kondetharayil Soman, A. 2023-04-01T07:00:00Z https://digitalcommons.uri.edu/gsofacpubs/2232 https://doi.org/10.1029/2022JC019083 unknown DigitalCommons@URI https://digitalcommons.uri.edu/gsofacpubs/2232 doi:10.1029/2022JC019083 https://doi.org/10.1029/2022JC019083 Graduate School of Oceanography Faculty Publications AMOC Nordic Seas overflows text 2023 ftunivrhodeislan https://doi.org/10.1029/2022JC019083 2024-01-15T19:10:03Z The Faroe-Bank Channel (FBC) is a key gateway through which dense overflow water of the Nordic Seas supplies the lower limb of the Atlantic Meridional Overturning Circulation. Most recently, it was discovered that a deep jet through the Faroe-Shetland Channel carries the bulk of this overflow water, but numerous questions regarding its structure, seasonality, and interannual variability as well as its linkage to atmospheric forcing remain poorly understood. A realistic high-resolution ocean reanalysis (GLORYS12; 1993–2018) is, therefore, employed to address these questions. We first confirm that the Faroe-Shetland Channel Jet is a permanent feature in GLORYS12 as well as in an ensemble of low-resolution reanalyses. On seasonal time scales, we find a strong transport covariability between this deep jet and the observed FBC overflow. On interannual time scales, the strength of this deep jet is governed by the wind-forced circulation in the Nordic Seas. Due to the largely barotropic structure of these flows, they have a signature detectable in satellite sea-surface heights. Further, we suggest that the structure of the deep jet is qualitatively consistent with a geostrophic dynamical model that accounts for along-isobath density variations. This study indicates that GLORYS12 is a promising product to study the dense water pathways and dynamics in the Nordic Seas. Text Nordic Seas University of Rhode Island: DigitalCommons@URI Faroe Bank ENVELOPE(-8.667,-8.667,60.917,60.917) Journal of Geophysical Research: Oceans 128 4 |
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University of Rhode Island: DigitalCommons@URI |
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ftunivrhodeislan |
language |
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topic |
AMOC Nordic Seas overflows |
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AMOC Nordic Seas overflows Chafik, L. Nilsson, J. Rossby, T. Kondetharayil Soman, A. The Faroe-Shetland Channel Jet: Structure, Variability, and Driving Mechanisms |
topic_facet |
AMOC Nordic Seas overflows |
description |
The Faroe-Bank Channel (FBC) is a key gateway through which dense overflow water of the Nordic Seas supplies the lower limb of the Atlantic Meridional Overturning Circulation. Most recently, it was discovered that a deep jet through the Faroe-Shetland Channel carries the bulk of this overflow water, but numerous questions regarding its structure, seasonality, and interannual variability as well as its linkage to atmospheric forcing remain poorly understood. A realistic high-resolution ocean reanalysis (GLORYS12; 1993–2018) is, therefore, employed to address these questions. We first confirm that the Faroe-Shetland Channel Jet is a permanent feature in GLORYS12 as well as in an ensemble of low-resolution reanalyses. On seasonal time scales, we find a strong transport covariability between this deep jet and the observed FBC overflow. On interannual time scales, the strength of this deep jet is governed by the wind-forced circulation in the Nordic Seas. Due to the largely barotropic structure of these flows, they have a signature detectable in satellite sea-surface heights. Further, we suggest that the structure of the deep jet is qualitatively consistent with a geostrophic dynamical model that accounts for along-isobath density variations. This study indicates that GLORYS12 is a promising product to study the dense water pathways and dynamics in the Nordic Seas. |
format |
Text |
author |
Chafik, L. Nilsson, J. Rossby, T. Kondetharayil Soman, A. |
author_facet |
Chafik, L. Nilsson, J. Rossby, T. Kondetharayil Soman, A. |
author_sort |
Chafik, L. |
title |
The Faroe-Shetland Channel Jet: Structure, Variability, and Driving Mechanisms |
title_short |
The Faroe-Shetland Channel Jet: Structure, Variability, and Driving Mechanisms |
title_full |
The Faroe-Shetland Channel Jet: Structure, Variability, and Driving Mechanisms |
title_fullStr |
The Faroe-Shetland Channel Jet: Structure, Variability, and Driving Mechanisms |
title_full_unstemmed |
The Faroe-Shetland Channel Jet: Structure, Variability, and Driving Mechanisms |
title_sort |
faroe-shetland channel jet: structure, variability, and driving mechanisms |
publisher |
DigitalCommons@URI |
publishDate |
2023 |
url |
https://digitalcommons.uri.edu/gsofacpubs/2232 https://doi.org/10.1029/2022JC019083 |
long_lat |
ENVELOPE(-8.667,-8.667,60.917,60.917) |
geographic |
Faroe Bank |
geographic_facet |
Faroe Bank |
genre |
Nordic Seas |
genre_facet |
Nordic Seas |
op_source |
Graduate School of Oceanography Faculty Publications |
op_relation |
https://digitalcommons.uri.edu/gsofacpubs/2232 doi:10.1029/2022JC019083 https://doi.org/10.1029/2022JC019083 |
op_doi |
https://doi.org/10.1029/2022JC019083 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
128 |
container_issue |
4 |
_version_ |
1790603356651126784 |