On the summer poleward coastal current off SW México

For the first time on the basis of direct observations (June 2003 and June 2005), the characteristics of the summer‐time coastal poleward current off SW Mexico are reported. Only the surface evidence of this coastal current has previously been described, from ship drift compilations. In June 2003 th...

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Bibliographic Details
Published in:Geophysical research letters Vol. 33; no. 2; pp. L02601 - n/a
Main Authors: Lavín, M. F., Beier, Emilio, Gómez-Valdés, José, Godínez, Víctor M., García, J.
Format: Journal Article
Language:English
Published: Washington, DC American Geophysical Union 01-01-2006
Blackwell Publishing Ltd
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Summary:For the first time on the basis of direct observations (June 2003 and June 2005), the characteristics of the summer‐time coastal poleward current off SW Mexico are reported. Only the surface evidence of this coastal current has previously been described, from ship drift compilations. In June 2003 the current was 90–180 km wide, 400 m deep, with speed ∼0.3 ms−1 and transport ∼4 Sv (1 Sv = 106 m3 s−1). In June 2005, its width was ∼90 km, it was 250–300 m deep, with mean speed ∼0.15 m s−1 and transport ∼2.5 Sv. California Current water (CCW) and equatorward flow were found further offshore. Mesoscale eddies significantly affected the coastal current, and transported CCW into the coastal zone.
Bibliography:ArticleID:2005GL024686
ark:/67375/WNG-2170MGL1-B
istex:89229FADFF2E54E474895DF8EEA846CD20BBF92F
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ISSN:0094-8276
1944-8007
DOI:10.1029/2005GL024686