Poleward intrusion in the northern Galician shelf

被引:4
作者
Alvarez, I. [2 ,3 ]
Ospina-Alvarez, N. [1 ]
deCastro, M. [2 ]
Varela, M. [4 ]
Gomez-Gesteira, M. [2 ]
Prego, R. [1 ]
机构
[1] CSIC, Marine Res Inst, Vigo 36208, Spain
[2] Univ Vigo, Fac Ciencias, EPhysLab, Orense 32004, Spain
[3] Univ Aveiro, Dept Fis, CESAM, P-3800 Aveiro, Portugal
[4] Ctr Oceanog La Coruna IEO, La Coruna, Spain
关键词
Iberian Poleward Current; Northern Galician Rias; SST; Ekman transport; thermohaline variables; nutrient salts; chlorophyll; NW IBERIAN PENINSULA; UPWELLING EVENT; WINTER; SPAIN; COAST; RIA; ATLANTIC; FRONTS; BISCAY; FLOWS;
D O I
10.1016/j.ecss.2010.02.009
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
The evolution of a warm water mass related to the Iberian Poleward Current (IPC) was characterized along the northern Galician shelf in November 2008 by means of Sea Surface Temperature and wind data. It was observed that under upwelling favorable conditions water temperature decreased along the northern coast and a temperature break appeared between Cape Vilano and Cape Ortegal showing a relaxation of the poleward intrusion. The effect of the IPC was also analyzed inside the Northern Galician Rias taking into account the hydrographical and biogeochemical properties measured on November 18. Water driven by the IPC was observed close to the mouth of the rias, around Cape Estaca de Bares, causing a nutrient salts decrease. Inside the rias a slight biological activity was found near surface resulting from fluvial contributions. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:545 / 552
页数:8
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