The Gulf of Cadiz Gap wind anticyclones

Autor: Xavier Carton, Dmitri Boutov, Ana Barbosa Aguiar, Álvaro Peliz
Přispěvatelé: Instituto Dom Luiz, Universidade de Lisboa (ULISBOA), Centro de Oceanographia, Laboratoire de physique des océans (LPO), Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)
Jazyk: angličtina
Rok vydání: 2014
Předmět:
Zdroj: Continental Shelf Research
Continental Shelf Research, Elsevier, 2014, 91, pp.171-191. ⟨10.1016/j.csr.2014.09.004⟩
ISSN: 0278-4343
1873-6955
Popis: International audience; We describe surface anticyclones developing in summer time after persistent Levanter (i.e., easterly) gap winds in the Gulf of Cadiz. The process of generation of these eddies is similar to those formed in the tropical Pacific eastern margin in many aspects, but their evolution and fate are different. The anticyclones are surface intensified structures with a radius of about 30 km, reach velocity maxima exceeding 30 cm/s, and have a strong baroclinic signature in the upper 150 m. They form when the thermocline is thin and shallow, after persistent easterly gap wind jets blowing through the Strait of Gibraltar. A conspicuous cold filament (nearly 8 °C negative anomaly), protruding seaward approximately aligned with the wind jet, is the first observable evidence of the phenomenon. An anticyclonic eddy is generated in the northern limb of the filament, and gradually acquires a rounded shape. No clear sign of a cyclonic counterpart is detected. The eddy remains trapped at the slope in close interaction with the Gulf of Cadiz slope Current (that feeds the Atlantic Inflow into the Mediterranean), and within a time-scale of 1–2 months the eddy dissipates by interaction with the Inflow and in some cases is swallowed into the Strait of Gibraltar. In 23 years (1991–2013) of satellite SST images we discovered 16 events (~0.7/yr). In a 20-yr simulation (1989–2008), 13 eddies were observed (~0.65/yr). The vast majority of eddies were observed in the August–October period. An event in 1997 is followed in SST imagery and with in situ hydrology data. This event is reproduced in the model in great detail and an analysis of its dynamics is presented.
Databáze: OpenAIRE
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