Wind stress mediated variability of the Filchner Trough overflow, Weddell Sea

The Filchner Trough (FT) is a key site for exchange of water masses between the Weddell Sea continental shelf and the deep ocean. Cold and dense Ice Shelf Water (ISW), a precursor for Antarctic Bottom Water, flows north along the FT and overflows the Filchner Sill. Although access of warm water to t...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Daae, Kjersti, Darelius, Elin Maria K., Fer, Ilker, Østerhus, Svein, Ryan, S.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2019
Subjects:
Online Access:https://hdl.handle.net/1956/20561
https://doi.org/10.1002/2017jc013579
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author Daae, Kjersti
Darelius, Elin Maria K.
Fer, Ilker
Østerhus, Svein
Ryan, S.
author_facet Daae, Kjersti
Darelius, Elin Maria K.
Fer, Ilker
Østerhus, Svein
Ryan, S.
author_sort Daae, Kjersti
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
container_issue 5
container_start_page 3186
container_title Journal of Geophysical Research: Oceans
container_volume 123
description The Filchner Trough (FT) is a key site for exchange of water masses between the Weddell Sea continental shelf and the deep ocean. Cold and dense Ice Shelf Water (ISW), a precursor for Antarctic Bottom Water, flows north along the FT and overflows the Filchner Sill. Although access of warm water to the Weddell Sea continental shelf is limited due to the presence of the Antarctic Slope Front, southward transport of warm water is facilitated through the FT. We use moored current meters from the Filchner Sill region to show that the monthly scale variability of the ISW overflow is connected to the variability of the alongslope wind stress upstream. Periods with significant correlation between the wind and ISW overflow are characterized by (I) wind directed along the continental slope, (II) high ISW overflow speed, and (III) high variability in the 16–64 day period band for wind and current. We propose that a recirculation of the slope current, associated with the Antarctic Slope Front, may occur in the FT during periods of strong wind forcing, and that such recirculation could explain the correlation between the wind stress and the ISW overflow. We further show that an increased wind stress along the continental slope leads to increased current speed within the slope current and the Antarctic Coastal Current, with possible implications for the on-shore heat transport. publishedVersion
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Ice Shelf
Weddell Sea
genre_facet Antarc*
Antarctic
Ice Shelf
Weddell Sea
geographic Antarctic
Filchner Trough
The Antarctic
Weddell
Weddell Sea
geographic_facet Antarctic
Filchner Trough
The Antarctic
Weddell
Weddell Sea
id ftunivbergen:oai:bora.uib.no:1956/20561
institution Open Polar
language English
long_lat ENVELOPE(-36.000,-36.000,-77.000,-77.000)
op_collection_id ftunivbergen
op_container_end_page 3203
op_doi https://doi.org/10.1002/2017jc013579
op_relation Norges forskningsråd: 211415
Norges forskningsråd: 231549
urn:issn:0148-0227
urn:issn:2156-2202
https://hdl.handle.net/1956/20561
https://doi.org/10.1002/2017jc013579
cristin:1581715
op_rights Attribution-Non Commercial-No Derivatives CC BY-NC-ND
http://creativecommons.org/licenses/by-nc-nd/4.0/
Copyright 2018 The Authors
op_source Journal of Geophysical Research
publishDate 2019
publisher American Geophysical Union
record_format openpolar
spelling ftunivbergen:oai:bora.uib.no:1956/20561 2025-01-16T19:25:42+00:00 Wind stress mediated variability of the Filchner Trough overflow, Weddell Sea Daae, Kjersti Darelius, Elin Maria K. Fer, Ilker Østerhus, Svein Ryan, S. 2019-01-24T09:03:58Z application/pdf https://hdl.handle.net/1956/20561 https://doi.org/10.1002/2017jc013579 eng eng American Geophysical Union Norges forskningsråd: 211415 Norges forskningsråd: 231549 urn:issn:0148-0227 urn:issn:2156-2202 https://hdl.handle.net/1956/20561 https://doi.org/10.1002/2017jc013579 cristin:1581715 Attribution-Non Commercial-No Derivatives CC BY-NC-ND http://creativecommons.org/licenses/by-nc-nd/4.0/ Copyright 2018 The Authors Journal of Geophysical Research VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 Peer reviewed Journal article 2019 ftunivbergen https://doi.org/10.1002/2017jc013579 2023-03-14T17:40:46Z The Filchner Trough (FT) is a key site for exchange of water masses between the Weddell Sea continental shelf and the deep ocean. Cold and dense Ice Shelf Water (ISW), a precursor for Antarctic Bottom Water, flows north along the FT and overflows the Filchner Sill. Although access of warm water to the Weddell Sea continental shelf is limited due to the presence of the Antarctic Slope Front, southward transport of warm water is facilitated through the FT. We use moored current meters from the Filchner Sill region to show that the monthly scale variability of the ISW overflow is connected to the variability of the alongslope wind stress upstream. Periods with significant correlation between the wind and ISW overflow are characterized by (I) wind directed along the continental slope, (II) high ISW overflow speed, and (III) high variability in the 16–64 day period band for wind and current. We propose that a recirculation of the slope current, associated with the Antarctic Slope Front, may occur in the FT during periods of strong wind forcing, and that such recirculation could explain the correlation between the wind stress and the ISW overflow. We further show that an increased wind stress along the continental slope leads to increased current speed within the slope current and the Antarctic Coastal Current, with possible implications for the on-shore heat transport. publishedVersion Article in Journal/Newspaper Antarc* Antarctic Ice Shelf Weddell Sea University of Bergen: Bergen Open Research Archive (BORA-UiB) Antarctic Filchner Trough ENVELOPE(-36.000,-36.000,-77.000,-77.000) The Antarctic Weddell Weddell Sea Journal of Geophysical Research: Oceans 123 5 3186 3203
spellingShingle VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452
VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452
Daae, Kjersti
Darelius, Elin Maria K.
Fer, Ilker
Østerhus, Svein
Ryan, S.
Wind stress mediated variability of the Filchner Trough overflow, Weddell Sea
title Wind stress mediated variability of the Filchner Trough overflow, Weddell Sea
title_full Wind stress mediated variability of the Filchner Trough overflow, Weddell Sea
title_fullStr Wind stress mediated variability of the Filchner Trough overflow, Weddell Sea
title_full_unstemmed Wind stress mediated variability of the Filchner Trough overflow, Weddell Sea
title_short Wind stress mediated variability of the Filchner Trough overflow, Weddell Sea
title_sort wind stress mediated variability of the filchner trough overflow, weddell sea
topic VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452
VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452
topic_facet VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452
VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452
url https://hdl.handle.net/1956/20561
https://doi.org/10.1002/2017jc013579