Observations of fresh, anticyclonic eddies in the Hudson Strait outflow
Author Posting. © The Author(s), 2010. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Journal of Marine Systems 88 (2011): 375-384, doi:10.1016/j.jmarsys.2010.12.004. Th...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/4903 2023-05-15T16:35:20+02:00 Observations of fresh, anticyclonic eddies in the Hudson Strait outflow Sutherland, David A. Straneo, Fiamma Lentz, Steven J. St-Laurent, Pierre 2010-07 application/pdf https://hdl.handle.net/1912/4903 en_US eng https://doi.org/10.1016/j.jmarsys.2010.12.004 https://hdl.handle.net/1912/4903 Hudson Strait Hudson Bay Labrador Current Freshwater Preprint 2010 ftwhoas https://doi.org/10.1016/j.jmarsys.2010.12.004 2022-05-28T22:58:29Z Author Posting. © The Author(s), 2010. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Journal of Marine Systems 88 (2011): 375-384, doi:10.1016/j.jmarsys.2010.12.004. The waters that flow out through Hudson Strait, a coastal system that connects Hudson Bay with the Labrador Sea, constitute the third largest freshwater contribution to the northern North Atlantic. Recent studies have documented the mean structure and transport of the outflow, as well as highlighting significant variability on synoptic scales (days–week). This study examines the outflow’s variability on these synoptic scales through the use of observations collected by a mooring array from 2005-2006. We focus on the mechanisms that cause the freshwater export to be concentrated in a series of discrete pulses during the fall/winter season. We find that the pulses occur once every 4.4 days on average and are associated with anticyclonic, surface-trapped eddies propagated through the strait by the mean outflow. Their occurrence is related to the passage of storms across Hudson Bay, although local instability processes also play a role in their formation. The eddies are responsible for approximately 40% of the mean volume transport and 50% of the mean freshwater transport out of the strait. We discuss the implications of this freshwater release mechanism on the delivery of nutrient-rich and highly stratified waters to the Labrador shelf, a productive region south of Hudson Strait. This work was funded by National Science Foundation grant OCE-0751554, with additional funding from the Office of Naval Research grant N00014-08-10490. Report Hudson Bay Hudson Strait Labrador Sea North Atlantic Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Hudson Hudson Bay Hudson Strait ENVELOPE(-70.000,-70.000,62.000,62.000) Labrador Shelf ENVELOPE(-58.000,-58.000,56.000,56.000) Journal of Marine Systems 88 3 375 384 |
institution |
Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
topic |
Hudson Strait Hudson Bay Labrador Current Freshwater |
spellingShingle |
Hudson Strait Hudson Bay Labrador Current Freshwater Sutherland, David A. Straneo, Fiamma Lentz, Steven J. St-Laurent, Pierre Observations of fresh, anticyclonic eddies in the Hudson Strait outflow |
topic_facet |
Hudson Strait Hudson Bay Labrador Current Freshwater |
description |
Author Posting. © The Author(s), 2010. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Journal of Marine Systems 88 (2011): 375-384, doi:10.1016/j.jmarsys.2010.12.004. The waters that flow out through Hudson Strait, a coastal system that connects Hudson Bay with the Labrador Sea, constitute the third largest freshwater contribution to the northern North Atlantic. Recent studies have documented the mean structure and transport of the outflow, as well as highlighting significant variability on synoptic scales (days–week). This study examines the outflow’s variability on these synoptic scales through the use of observations collected by a mooring array from 2005-2006. We focus on the mechanisms that cause the freshwater export to be concentrated in a series of discrete pulses during the fall/winter season. We find that the pulses occur once every 4.4 days on average and are associated with anticyclonic, surface-trapped eddies propagated through the strait by the mean outflow. Their occurrence is related to the passage of storms across Hudson Bay, although local instability processes also play a role in their formation. The eddies are responsible for approximately 40% of the mean volume transport and 50% of the mean freshwater transport out of the strait. We discuss the implications of this freshwater release mechanism on the delivery of nutrient-rich and highly stratified waters to the Labrador shelf, a productive region south of Hudson Strait. This work was funded by National Science Foundation grant OCE-0751554, with additional funding from the Office of Naval Research grant N00014-08-10490. |
format |
Report |
author |
Sutherland, David A. Straneo, Fiamma Lentz, Steven J. St-Laurent, Pierre |
author_facet |
Sutherland, David A. Straneo, Fiamma Lentz, Steven J. St-Laurent, Pierre |
author_sort |
Sutherland, David A. |
title |
Observations of fresh, anticyclonic eddies in the Hudson Strait outflow |
title_short |
Observations of fresh, anticyclonic eddies in the Hudson Strait outflow |
title_full |
Observations of fresh, anticyclonic eddies in the Hudson Strait outflow |
title_fullStr |
Observations of fresh, anticyclonic eddies in the Hudson Strait outflow |
title_full_unstemmed |
Observations of fresh, anticyclonic eddies in the Hudson Strait outflow |
title_sort |
observations of fresh, anticyclonic eddies in the hudson strait outflow |
publishDate |
2010 |
url |
https://hdl.handle.net/1912/4903 |
long_lat |
ENVELOPE(-70.000,-70.000,62.000,62.000) ENVELOPE(-58.000,-58.000,56.000,56.000) |
geographic |
Hudson Hudson Bay Hudson Strait Labrador Shelf |
geographic_facet |
Hudson Hudson Bay Hudson Strait Labrador Shelf |
genre |
Hudson Bay Hudson Strait Labrador Sea North Atlantic |
genre_facet |
Hudson Bay Hudson Strait Labrador Sea North Atlantic |
op_relation |
https://doi.org/10.1016/j.jmarsys.2010.12.004 https://hdl.handle.net/1912/4903 |
op_doi |
https://doi.org/10.1016/j.jmarsys.2010.12.004 |
container_title |
Journal of Marine Systems |
container_volume |
88 |
container_issue |
3 |
container_start_page |
375 |
op_container_end_page |
384 |
_version_ |
1766025553245110272 |