Ekman transport patterns in the area close to the Galician coast (NW, Spain)
A 40 year time series of daily and monthly Ekman transport is analysed in an oceanic area 150 km offshore Cape Finisterre (43°N, 11°W). The periodicity of the signal showed an annual component (365 days), a seasonal fluctuation (50 days) and a time scale related to passing storms (20 days). The Ekma...
| Autores: | , |
|---|---|
| Formato: | artículo |
| Fecha de publicación: | 2006 |
| País: | España |
| Recursos: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/324166 |
| Acesso em linha: | http://hdl.handle.net/10261/324166 |
| Access Level: | acceso abierto |
| Palavra-chave: | Centro Oceanográfico de Vigo Medio Marino |
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Ekman transport patterns in the area close to the Galician coast (NW, Spain)Cabanas-López, José ManuelÁlvarez, I.Centro Oceanográfico de VigoMedio MarinoA 40 year time series of daily and monthly Ekman transport is analysed in an oceanic area 150 km offshore Cape Finisterre (43°N, 11°W). The periodicity of the signal showed an annual component (365 days), a seasonal fluctuation (50 days) and a time scale related to passing storms (20 days). The Ekman transport showed different seasonal patterns. Thus, the summer pattern is characterized by transport pointing seaward (upwelling favourable) practically perpendicular to the shoreline, while the winter pattern is characterized by transport pointing landward (downwelling favourable). Although the most favourable upwelling conditions were observed during summer, for the last 15 years the frequency of observed winter upwelling events is higher due to the prevalence of northerly winds.Sí202320232006info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501http://hdl.handle.net/10261/324166reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)InglésCentro Oceanográfico de Vigoinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/3241662026-05-22T06:33:51Z |
| dc.title.none.fl_str_mv |
Ekman transport patterns in the area close to the Galician coast (NW, Spain) |
| title |
Ekman transport patterns in the area close to the Galician coast (NW, Spain) |
| spellingShingle |
Ekman transport patterns in the area close to the Galician coast (NW, Spain) Cabanas-López, José Manuel Centro Oceanográfico de Vigo Medio Marino |
| title_short |
Ekman transport patterns in the area close to the Galician coast (NW, Spain) |
| title_full |
Ekman transport patterns in the area close to the Galician coast (NW, Spain) |
| title_fullStr |
Ekman transport patterns in the area close to the Galician coast (NW, Spain) |
| title_full_unstemmed |
Ekman transport patterns in the area close to the Galician coast (NW, Spain) |
| title_sort |
Ekman transport patterns in the area close to the Galician coast (NW, Spain) |
| dc.creator.none.fl_str_mv |
Cabanas-López, José Manuel Álvarez, I. |
| author |
Cabanas-López, José Manuel |
| author_facet |
Cabanas-López, José Manuel Álvarez, I. |
| author_role |
author |
| author2 |
Álvarez, I. |
| author2_role |
author |
| dc.subject.none.fl_str_mv |
Centro Oceanográfico de Vigo Medio Marino |
| topic |
Centro Oceanográfico de Vigo Medio Marino |
| description |
A 40 year time series of daily and monthly Ekman transport is analysed in an oceanic area 150 km offshore Cape Finisterre (43°N, 11°W). The periodicity of the signal showed an annual component (365 days), a seasonal fluctuation (50 days) and a time scale related to passing storms (20 days). The Ekman transport showed different seasonal patterns. Thus, the summer pattern is characterized by transport pointing seaward (upwelling favourable) practically perpendicular to the shoreline, while the winter pattern is characterized by transport pointing landward (downwelling favourable). Although the most favourable upwelling conditions were observed during summer, for the last 15 years the frequency of observed winter upwelling events is higher due to the prevalence of northerly winds. |
| publishDate |
2006 |
| dc.date.none.fl_str_mv |
2006 2023 2023 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 |
| format |
article |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10261/324166 |
| url |
http://hdl.handle.net/10261/324166 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
Centro Oceanográfico de Vigo |
| dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
| eu_rights_str_mv |
openAccess |
| dc.source.none.fl_str_mv |
reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
| instname_str |
Consejo Superior de Investigaciones Científicas (CSIC) |
| reponame_str |
DIGITAL.CSIC. Repositorio Institucional del CSIC |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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1869407866643808256 |
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15,811543 |