Cyclonic eddies in the West Greenland boundary current system
The boundary current system in the Labrador Sea plays an integral role in modulating convection in the interior basin. Four years of mooring data from the eastern Labrador Sea reveal persistent mesoscale variability in the West Greenland boundary current. Between 2014 and 2018, 197 mid-depth intensi...
Published in: | Journal of Physical Oceanography |
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Language: | English |
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American Meteorological Society
2021
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Online Access: | http://nora.nerc.ac.uk/id/eprint/530376/ https://nora.nerc.ac.uk/id/eprint/530376/1/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20Cyclonic%20Eddies%20in%20the%20West%20Greenland%20Boundary%20Current%20System%20%282%29.pdf https://doi.org/10.1175/JPO-D-20-0255.1 |
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ftnerc:oai:nora.nerc.ac.uk:530376 2023-05-15T15:51:49+02:00 Cyclonic eddies in the West Greenland boundary current system Pacini, Astrid Pickart, Robert S. Le Bras, Isabela A. Straneo, Fiammetta Holliday, N.P. Spall, M.A. 2021-06-08 text http://nora.nerc.ac.uk/id/eprint/530376/ https://nora.nerc.ac.uk/id/eprint/530376/1/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20Cyclonic%20Eddies%20in%20the%20West%20Greenland%20Boundary%20Current%20System%20%282%29.pdf https://doi.org/10.1175/JPO-D-20-0255.1 en eng American Meteorological Society https://nora.nerc.ac.uk/id/eprint/530376/1/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20Cyclonic%20Eddies%20in%20the%20West%20Greenland%20Boundary%20Current%20System%20%282%29.pdf Pacini, Astrid; Pickart, Robert S.; Le Bras, Isabela A.; Straneo, Fiammetta; Holliday, N.P. orcid:0000-0002-9733-8002 Spall, M.A. 2021 Cyclonic eddies in the West Greenland boundary current system. Journal of Physical Oceanography. https://doi.org/10.1175/JPO-D-20-0255.1 <https://doi.org/10.1175/JPO-D-20-0255.1> Publication - Article PeerReviewed 2021 ftnerc https://doi.org/10.1175/JPO-D-20-0255.1 2023-02-04T19:52:08Z The boundary current system in the Labrador Sea plays an integral role in modulating convection in the interior basin. Four years of mooring data from the eastern Labrador Sea reveal persistent mesoscale variability in the West Greenland boundary current. Between 2014 and 2018, 197 mid-depth intensified cyclones were identified that passed the array near the 2000 m isobath. In this study, we quantify these features and show that they are the downstream manifestation of Denmark Strait Overflow Water (DSOW) cyclones. A composite cyclone is constructed revealing an average radius of 9 km, maximum azimuthal speed of 24 cm/s, and a core propagation velocity of 27 cm/s. The core propagation velocity is significantly smaller than upstream near Denmark Strait, allowing them to trap more water. The cyclones transport a 200-m thick lens of dense water at the bottom of the water column, and increase the transport of DSOW in the West Greenland boundary current by 17% relative to the background flow. Only a portion of the features generated at Denmark Strait make it to the Labrador Sea, implying that the remainder are shed into the interior Irminger Sea, are retroflected at Cape Farewell, or dissipate. A synoptic shipboard survey east of Cape Farewell, conducted in summer 2020, captured two of these features which shed further light on their structure and timing. This is the first time DSOW cyclones have been observed in the Labrador Sea—a discovery that could have important implications for interior stratification. Article in Journal/Newspaper Cape Farewell Denmark Strait Greenland Labrador Sea Natural Environment Research Council: NERC Open Research Archive Greenland Irminger Sea ENVELOPE(-34.041,-34.041,63.054,63.054) Journal of Physical Oceanography |
institution |
Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
English |
description |
The boundary current system in the Labrador Sea plays an integral role in modulating convection in the interior basin. Four years of mooring data from the eastern Labrador Sea reveal persistent mesoscale variability in the West Greenland boundary current. Between 2014 and 2018, 197 mid-depth intensified cyclones were identified that passed the array near the 2000 m isobath. In this study, we quantify these features and show that they are the downstream manifestation of Denmark Strait Overflow Water (DSOW) cyclones. A composite cyclone is constructed revealing an average radius of 9 km, maximum azimuthal speed of 24 cm/s, and a core propagation velocity of 27 cm/s. The core propagation velocity is significantly smaller than upstream near Denmark Strait, allowing them to trap more water. The cyclones transport a 200-m thick lens of dense water at the bottom of the water column, and increase the transport of DSOW in the West Greenland boundary current by 17% relative to the background flow. Only a portion of the features generated at Denmark Strait make it to the Labrador Sea, implying that the remainder are shed into the interior Irminger Sea, are retroflected at Cape Farewell, or dissipate. A synoptic shipboard survey east of Cape Farewell, conducted in summer 2020, captured two of these features which shed further light on their structure and timing. This is the first time DSOW cyclones have been observed in the Labrador Sea—a discovery that could have important implications for interior stratification. |
format |
Article in Journal/Newspaper |
author |
Pacini, Astrid Pickart, Robert S. Le Bras, Isabela A. Straneo, Fiammetta Holliday, N.P. Spall, M.A. |
spellingShingle |
Pacini, Astrid Pickart, Robert S. Le Bras, Isabela A. Straneo, Fiammetta Holliday, N.P. Spall, M.A. Cyclonic eddies in the West Greenland boundary current system |
author_facet |
Pacini, Astrid Pickart, Robert S. Le Bras, Isabela A. Straneo, Fiammetta Holliday, N.P. Spall, M.A. |
author_sort |
Pacini, Astrid |
title |
Cyclonic eddies in the West Greenland boundary current system |
title_short |
Cyclonic eddies in the West Greenland boundary current system |
title_full |
Cyclonic eddies in the West Greenland boundary current system |
title_fullStr |
Cyclonic eddies in the West Greenland boundary current system |
title_full_unstemmed |
Cyclonic eddies in the West Greenland boundary current system |
title_sort |
cyclonic eddies in the west greenland boundary current system |
publisher |
American Meteorological Society |
publishDate |
2021 |
url |
http://nora.nerc.ac.uk/id/eprint/530376/ https://nora.nerc.ac.uk/id/eprint/530376/1/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20Cyclonic%20Eddies%20in%20the%20West%20Greenland%20Boundary%20Current%20System%20%282%29.pdf https://doi.org/10.1175/JPO-D-20-0255.1 |
long_lat |
ENVELOPE(-34.041,-34.041,63.054,63.054) |
geographic |
Greenland Irminger Sea |
geographic_facet |
Greenland Irminger Sea |
genre |
Cape Farewell Denmark Strait Greenland Labrador Sea |
genre_facet |
Cape Farewell Denmark Strait Greenland Labrador Sea |
op_relation |
https://nora.nerc.ac.uk/id/eprint/530376/1/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20Cyclonic%20Eddies%20in%20the%20West%20Greenland%20Boundary%20Current%20System%20%282%29.pdf Pacini, Astrid; Pickart, Robert S.; Le Bras, Isabela A.; Straneo, Fiammetta; Holliday, N.P. orcid:0000-0002-9733-8002 Spall, M.A. 2021 Cyclonic eddies in the West Greenland boundary current system. Journal of Physical Oceanography. https://doi.org/10.1175/JPO-D-20-0255.1 <https://doi.org/10.1175/JPO-D-20-0255.1> |
op_doi |
https://doi.org/10.1175/JPO-D-20-0255.1 |
container_title |
Journal of Physical Oceanography |
_version_ |
1766387204210294784 |