“…It should be noted that in the ADCP current meter was deployed at 40 m depth in the study of the Carter et al, 1979;Walters and Gartner, 1985;Valle Levinson et al, 1998;Wong and Moses-Hall, 1998;Wong and DiLorenzo, 1988;Wong, 2002). The effect of coastal winds is specially relevant in areas affected by permanent or seasonal upwelling, as it is the case of the Galician rías (Rosón et al, 1997;Álvarez-Salgado et al, 2000;Pardo et al, 2001), the Chilean fjords (Aysen Fjord, Cáceres et al, 2002) or Bantry Bay in South West Ireland (Edwards et al, 1996). Similarly high percentages of the subtidal current variability explained by coastal winds have been found in the Ría de Vigo (>65%; Piedracoba et al, 2005), the Ría de Arousa (50%; Rosón et al, 1997) (Rosón et al, 1997;Álvarez-Salgado et al, 2000).…”