Mesoscale variability in the Alboran Sea: Synthetic aperture radar imaging of frontal eddies
17 pages, 16 figures
| Autores: | , , , , |
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| Formato: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2002 |
| País: | España |
| Recursos: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/408629 |
| Acesso em linha: | http://hdl.handle.net/10261/408629 |
| Access Level: | acceso abierto |
| Palavra-chave: | Ocean mesoscale SAR Alboran Sea Western Mediterranean Sea Surface layer circulation |
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Mesoscale variability in the Alboran Sea: Synthetic aperture radar imaging of frontal eddiesFont, JordiRousseau, StéphanShirasago Germán, BernardoGarcia-Gorriz, ElisaHaney, Robert L.Ocean mesoscaleSARAlboran SeaWestern Mediterranean SeaSurface layer circulation17 pages, 16 figuresIn autumn 1992 the entire Alboran Sea (western Mediterranean) was sampled by the Spanish R/V García del Cid. The incoming jet of Atlantic water, its associated meandering front, and the two big anticyclonic gyres were described from conductivity-temperature-depth (CTD) and acoustic Doppler current profiler (ADCP) data. Smaller-scale eddies were also observed. Additionally, 36 ERS-1 synthetic aperture radar (SAR) scenes were obtained from mid-September to mid-October. The SAR images capture these features when wind conditions are suitable. The current shear is mainly depicted as narrow lines of low backscatter because of the damping of waves by natural surface films. These lines delineate the northern border of both gyres and the beginning of the alongslope Algerian current at the eastern limit of the Alboran Sea. ADCP observations confirm that lines on SAR imagery follow the direction of the surface currents. The two gyres present high backscatter values in their center, while their frontal boundaries appear modulated by the variation of the marine atmospheric boundary layer stratification due to the surface thermal front. SAR has observed small spiral eddies that were not evidenced by the almost contemporaneous but too coarse CTD in situ sampling. Good spatial correspondence between radar-detected and in situ-measured structures occurs when comparing SAR images to the surface dynamic topography, rather than strictly surface water characteristicsPeer reviewedAmerican Geophysical UnionConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]202520252002info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Publisher's versioninfo:eu-repo/semantics/publishedVersionhttp://hdl.handle.net/10261/408629reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Ingléshttps://doi.org/10.1029/2001JC000835Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/4086292026-05-22T06:33:51Z |
| dc.title.none.fl_str_mv |
Mesoscale variability in the Alboran Sea: Synthetic aperture radar imaging of frontal eddies |
| title |
Mesoscale variability in the Alboran Sea: Synthetic aperture radar imaging of frontal eddies |
| spellingShingle |
Mesoscale variability in the Alboran Sea: Synthetic aperture radar imaging of frontal eddies Font, Jordi Ocean mesoscale SAR Alboran Sea Western Mediterranean Sea Surface layer circulation |
| title_short |
Mesoscale variability in the Alboran Sea: Synthetic aperture radar imaging of frontal eddies |
| title_full |
Mesoscale variability in the Alboran Sea: Synthetic aperture radar imaging of frontal eddies |
| title_fullStr |
Mesoscale variability in the Alboran Sea: Synthetic aperture radar imaging of frontal eddies |
| title_full_unstemmed |
Mesoscale variability in the Alboran Sea: Synthetic aperture radar imaging of frontal eddies |
| title_sort |
Mesoscale variability in the Alboran Sea: Synthetic aperture radar imaging of frontal eddies |
| dc.creator.none.fl_str_mv |
Font, Jordi Rousseau, Stéphan Shirasago Germán, Bernardo Garcia-Gorriz, Elisa Haney, Robert L. |
| author |
Font, Jordi |
| author_facet |
Font, Jordi Rousseau, Stéphan Shirasago Germán, Bernardo Garcia-Gorriz, Elisa Haney, Robert L. |
| author_role |
author |
| author2 |
Rousseau, Stéphan Shirasago Germán, Bernardo Garcia-Gorriz, Elisa Haney, Robert L. |
| author2_role |
author author author author |
| dc.contributor.none.fl_str_mv |
Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72] |
| dc.subject.none.fl_str_mv |
Ocean mesoscale SAR Alboran Sea Western Mediterranean Sea Surface layer circulation |
| topic |
Ocean mesoscale SAR Alboran Sea Western Mediterranean Sea Surface layer circulation |
| description |
17 pages, 16 figures |
| publishDate |
2002 |
| dc.date.none.fl_str_mv |
2002 2025 2025 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 Publisher's version info:eu-repo/semantics/publishedVersion |
| format |
article |
| status_str |
publishedVersion |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10261/408629 |
| url |
http://hdl.handle.net/10261/408629 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
https://doi.org/10.1029/2001JC000835 Sí |
| dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
| eu_rights_str_mv |
openAccess |
| dc.publisher.none.fl_str_mv |
American Geophysical Union |
| publisher.none.fl_str_mv |
American Geophysical Union |
| 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 |
| collection |
DIGITAL.CSIC. Repositorio Institucional del CSIC |
| repository.name.fl_str_mv |
|
| repository.mail.fl_str_mv |
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| _version_ |
1869414028071141376 |
| score |
15,81155 |