The potential vorticity flux through the Yucatan Channel and the Loop Current in the Gulf of Mexico

Two‐year‐long time series of current and density structure measurements across the Yucatan Channel's main section allow the calculation of the time‐dependent potential vorticity flux between the Gulf of Mexico and the Caribbean Sea, which is characterized by alternating periods of positive (cyc...

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Bibliographic Details
Published inGeophysical research letters Vol. 29; no. 22; pp. 16-1 - 16-4
Main Authors Candela, Julio, Sheinbaum, Julio, Ochoa, José, Badan, Antoine, Leben, Robert
Format Journal Article
LanguageEnglish
Published American Geophysical Union 01.11.2002
Blackwell Publishing Ltd
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Summary:Two‐year‐long time series of current and density structure measurements across the Yucatan Channel's main section allow the calculation of the time‐dependent potential vorticity flux between the Gulf of Mexico and the Caribbean Sea, which is characterized by alternating periods of positive (cyclonic) and negative (anti‐cyclonic) vorticity influx. Periods of negative cumulative vorticity influx are related to the Loop Current extending into the Gulf of Mexico, whereas periods of positive cumulative vorticity influx relate to a Loop Current retraction, sometimes coincident with the shedding of an anti‐cyclonic eddy.
Bibliography:ark:/67375/WNG-L8RV7HRX-W
ArticleID:2002GL015587
istex:1789612F6AC1C028CB04FE28AC11E8AE85B49C15
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0094-8276
1944-8007
DOI:10.1029/2002GL015587