globalchange  > 过去全球变化的重建
DOI: 10.1016/j.marpolbul.2014.01.036
Scopus记录号: 2-s2.0-84896395626
论文题名:
Meteorologically-driven circulation and flushing times of the Bay of Algeciras, Strait of Gibraltar
作者: Sánchez-Garrido J.C.; Lafuente J.G.; Sammartino S.; Naranjo C.; de los Santos F.J.; Álvarez Fanjul E.
刊名: Marine Pollution Bulletin
ISSN: 0025-326X
EISSN: 1879-3363
出版年: 2014
卷: 80, 期:2018-01-02
起始页码: 97
结束页码: 106
语种: 英语
英文关键词: Bay of Algeciras ; E-Flushing time ; MITgcm ; Tidal flushing ; Wind-driven circulation
Scopus关键词: Bay of Algeciras ; E-Flushing time ; MITgcm ; Tidal flushing ; Wind-driven circulation ; Contamination ; Marine pollution ; Atmospheric pressure ; surface water ; flushing ; Mediterranean Water ; meteorology ; ocean tide ; oceanic circulation ; wind forcing ; wind-driven circulation ; acceleration ; article ; Atlantic Ocean ; atmospheric pressure ; deceleration ; Mediterranean Sea ; seasonal variation ; tidal flushing ; tide ; water flow ; water transport ; wind ; wind driven circulation ; Bay of Algeciras ; e-Flushing time ; MITgcm ; Tidal flushing ; Wind-driven circulation ; Bays ; Environmental Monitoring ; Gibraltar ; Meteorological Concepts ; Seawater ; Water Movements ; Algeciras Bay ; Andalucia ; Cadiz [Andalucia] ; Spain ; Strait of Gibraltar ; Bay of Algeciras ; e-Flushing time ; MITgcm ; Tidal flushing ; Wind-driven circulation
Scopus学科分类: Agricultural and Biological Sciences: Aquatic Science ; Earth and Planetary Sciences: Oceanography ; Environmental Science: Pollution
英文摘要: A primitive-equation model has been used to investigate the meteorologically-driven circulation of the Bay of Algeciras. It is shown that the mean circulation of Atlantic Water (AW) is characterized by an anticyclonic cell, while Mediterranean Water (MW) follows a preferred cyclonic pathway. Meteorological forcing distorts substantially the AW mean circulation pattern, and only modulates that of the MW. Winds drive a vertical circulation cell in the Atlantic layer consistent with Ekman dynamics, whereas the horizontal circulation pattern is markedly dependent on the swift Atlantic jet entering the Mediterranean and changes from clearly anticyclonic to cyclonic as the jet separates or approaches the strait's northern shoreline. This occurs through atmospheric pressure-driven acceleration/deceleration of the jet, in agreement with internal hydraulics theory predictions. It is also found that the renewal of AW is largely modulated by tides, with meteorological forcing playing a secondary role. The opposite applies to the renewal of MW. © 2014 Elsevier Ltd.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/85649
Appears in Collections:过去全球变化的重建
全球变化的国际研究计划

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作者单位: Physical Oceanography Group, University of Málaga, Campus de Teatinos s/n, 29071 Málaga, Spain; Autoridad Portuaria Bahía de Algeciras, Avda. de la Hispanidad 2, 11207 Algeciras, Cádiz, Spain; Puertos del Estado, Avda. del Partenón 10, 28042 Madrid, Spain

Recommended Citation:
Sánchez-Garrido J.C.,Lafuente J.G.,Sammartino S.,et al. Meteorologically-driven circulation and flushing times of the Bay of Algeciras, Strait of Gibraltar[J]. Marine Pollution Bulletin,2014-01-01,80(2018-01-02)
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