Geostrophic and ageostrophic circulation of a shallow anticyclonic eddy off Cape Bojador

Author:

Ruiz Simón1,Pelegrí Josep L.2,Emelianov Mikhail2,Pascual Ananda1,Mason Evan1

Affiliation:

1. Instituto Mediterráneo de Estudios Avanzados (CSIC-UIB); Department of Marine Tecnologies, Operational Oceanography and Sustainability, Esporles Spain

2. Institut de Ciències del Mar; Department of Physical and Technological Oceanography, CSIC, Passeig Maritim de la Barceloneta; Barcelona Spain

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Reference48 articles.

1. Mesoscale subduction at the Almeria-Oran front: Part 1: Agesotrophic flow;Allen;J. Mar. Syst.,2001

2. Island-induced eddies in the Canary Islands;Arístegui;Deep Sea Res., Part I,1994

3. The influence of island-generated eddies on chlorophyll distribution: A study of mesoscale variation around Gran Canaria;Arístegui;Deep Sea Res., Part I,1997

4. Barton , E. D. 1998 The Sea A. R. Robinson K. H. Brink 633 657 John Wiley New York

5. The transition zone of the Canary Current upwelling region;Barton;Prog. Oceanogr.,1998

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