English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/90141
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE
Exportar a otros formatos:


Wind-driven surface circulation in the Cape Blanc region

AuthorsCastellanos, Paola ; Pelegrí, Josep Lluís ; Benazzouz, Aïssa
KeywordsSurface currents
Tracking structures
Cape Blanc
Coastal upwelling
Issue DateJun-2013
PublisherPergamon Press
CitationContinental Shelf Research 60: 87-103 (2013)
AbstractWe analyze the short-term transition, on time scales of the order of days and weeks, of the surface fields in the coastal transition zone off Northwest Africa, between 15°N and 25°N, during winter and spring 2005 and 2006. This is a complex region characterized by the baroclinic coastal jet north of Cape Blanc, along-shore convergence and water export at the Cape Blanc giant filament, and substantial mesoscale variability between Capes Verde and Blanc. We use the anomalies of the wind impulse and two different coastal upwelling indexes, evaluated off 17°N, 20°N and 23°N, in order to assess the importance of wind forcing in this short-term variability. We also employ daily and weekly surface maps of wind, temperature, surface height and currents to investigate which are the mechanisms that lead to the relatively fast changes in the flow patterns. The coastal baroclinic jet and the Cape Blanc giant filament are ubiquitous features, the two being intrinsically related through the intensity of upwelling off Cape Blanc. Therefore, the strength of both features responds, to a large extent, to the fluctuations of the northeasterly winds; their intensity is greater in spring than winter but during both seasons they experience relatively fast oscillations related to the intermittency of the wind field. The mesoscalar features are visible in the entire domain, with time scales typically of the order of two weeks, but become prominent in the southern region during spring, apparently related to an intense northward coastal jet south of Cape Blanc. © 2013 Elsevier Ltd.
Description17 pages, 14 figures, 2 tables
Publisher version (URL)https://doi.org/10.1016/j.csr.2013.02.003
Identifiersdoi: 10.1016/j.csr.2013.02.003
issn: 0278-4343
e-issn: 1873-6955
Appears in Collections:(ICM) Artículos
Files in This Item:
There are no files associated with this item.
Show full item record
Review this work

Related articles:

WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.