Effects of winds and Caribbean eddies on the frequency of Loop Current eddy shedding: A numerical model study
[1] The Loop Current (LC) is known to shed eddies at irregular intervals from 3 to 17 months. The causes of this irregularity have not, however, been adequately identified previously. We examine the effects of various types of external forcing on shedding with a model of the western North Atlantic O...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.586.3295 2023-05-15T17:34:08+02:00 Effects of winds and Caribbean eddies on the frequency of Loop Current eddy shedding: A numerical model study L. -y. Oey H. -c. Lee William J. Schmitz The Pennsylvania State University CiteSeerX Archives 2003 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.586.3295 http://www.aos.princeton.edu/WWWPUBLIC/PROFS/PUBLICATION/oey_lee_schmitz.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.586.3295 http://www.aos.princeton.edu/WWWPUBLIC/PROFS/PUBLICATION/oey_lee_schmitz.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.aos.princeton.edu/WWWPUBLIC/PROFS/PUBLICATION/oey_lee_schmitz.pdf Gulf of Mexico Caribbean Current Loop Current eddy shedding winds and eddies numerical ocean model text 2003 ftciteseerx 2016-01-08T13:16:54Z [1] The Loop Current (LC) is known to shed eddies at irregular intervals from 3 to 17 months. The causes of this irregularity have not, however, been adequately identified previously. We examine the effects of various types of external forcing on shedding with a model of the western North Atlantic Ocean (96–55W, 6–50N). We force the model with steady transport at 55W, with winds, and include eddies in the Caribbean Sea. We examine their separate effects. With steady transport only, the model sheds rings at a dominant period of 9–10 months. Wind-induced transport fluctuations through the Greater Antilles Passages cause shedding at shorter intervals (3–7 months). Caribbean eddies (anticyclones) cause shedding at longer periods (14–16 months). Potential vorticity conservation indicates that Caribbean eddies tend to deter northward extension of the LC into the Gulf, which can lead to longer periods between eddy shedding. Fluctuating inflow at the Yucatan Channel that is associated with winds and/or Caribbean eddies can cause an LC eddy to temporarily (1 month) detach from and then reattach back to the LC, a phenomenon often observed. Model results also suggest that southwest of Hispaniola, warm eddies are spun up by the local wind stress curl. This type of eddy drifts Text North Atlantic Unknown Curl ENVELOPE(-63.071,-63.071,-70.797,-70.797) |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
topic |
Gulf of Mexico Caribbean Current Loop Current eddy shedding winds and eddies numerical ocean model |
spellingShingle |
Gulf of Mexico Caribbean Current Loop Current eddy shedding winds and eddies numerical ocean model L. -y. Oey H. -c. Lee William J. Schmitz Effects of winds and Caribbean eddies on the frequency of Loop Current eddy shedding: A numerical model study |
topic_facet |
Gulf of Mexico Caribbean Current Loop Current eddy shedding winds and eddies numerical ocean model |
description |
[1] The Loop Current (LC) is known to shed eddies at irregular intervals from 3 to 17 months. The causes of this irregularity have not, however, been adequately identified previously. We examine the effects of various types of external forcing on shedding with a model of the western North Atlantic Ocean (96–55W, 6–50N). We force the model with steady transport at 55W, with winds, and include eddies in the Caribbean Sea. We examine their separate effects. With steady transport only, the model sheds rings at a dominant period of 9–10 months. Wind-induced transport fluctuations through the Greater Antilles Passages cause shedding at shorter intervals (3–7 months). Caribbean eddies (anticyclones) cause shedding at longer periods (14–16 months). Potential vorticity conservation indicates that Caribbean eddies tend to deter northward extension of the LC into the Gulf, which can lead to longer periods between eddy shedding. Fluctuating inflow at the Yucatan Channel that is associated with winds and/or Caribbean eddies can cause an LC eddy to temporarily (1 month) detach from and then reattach back to the LC, a phenomenon often observed. Model results also suggest that southwest of Hispaniola, warm eddies are spun up by the local wind stress curl. This type of eddy drifts |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
L. -y. Oey H. -c. Lee William J. Schmitz |
author_facet |
L. -y. Oey H. -c. Lee William J. Schmitz |
author_sort |
L. -y. Oey |
title |
Effects of winds and Caribbean eddies on the frequency of Loop Current eddy shedding: A numerical model study |
title_short |
Effects of winds and Caribbean eddies on the frequency of Loop Current eddy shedding: A numerical model study |
title_full |
Effects of winds and Caribbean eddies on the frequency of Loop Current eddy shedding: A numerical model study |
title_fullStr |
Effects of winds and Caribbean eddies on the frequency of Loop Current eddy shedding: A numerical model study |
title_full_unstemmed |
Effects of winds and Caribbean eddies on the frequency of Loop Current eddy shedding: A numerical model study |
title_sort |
effects of winds and caribbean eddies on the frequency of loop current eddy shedding: a numerical model study |
publishDate |
2003 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.586.3295 http://www.aos.princeton.edu/WWWPUBLIC/PROFS/PUBLICATION/oey_lee_schmitz.pdf |
long_lat |
ENVELOPE(-63.071,-63.071,-70.797,-70.797) |
geographic |
Curl |
geographic_facet |
Curl |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
http://www.aos.princeton.edu/WWWPUBLIC/PROFS/PUBLICATION/oey_lee_schmitz.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.586.3295 http://www.aos.princeton.edu/WWWPUBLIC/PROFS/PUBLICATION/oey_lee_schmitz.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766132870542262272 |