Author/Authors :
ءlvarez-Salgado، نويسنده , , X.A and Figueiras، نويسنده , , F.G and Pérez، نويسنده , , F.F. and Groom، نويسنده , , S and Nogueira، نويسنده , , E and Borges، نويسنده , , A.V and Chou، نويسنده , , L and Castro، نويسنده , , C.G and Moncoiffé، نويسنده , , G and Rيos، نويسنده , , A.F. and Miller، نويسنده , , A.E.J and Frankignoulle، نويسنده , , M and Savidge، نويسنده , , G and Wollast، نويسنده , , R، نويسنده ,
Abstract :
Time series of wind-stress data, AVHRR and SeaWiFS satellite images, and in situ data from seven cruises are used to assemble a coherent picture of the hydrographic variability of the seas off the Northwest Iberian Peninsula from the onset (September–October) to the cessation (February–May) of the Portugal coastal counter current (PCCC). During this period the chemistry and the biology of the shelf, slope and ocean waters between 40° and 43°N have previously been undersampled. Novel information extracted from these observations relate to:1.
st frequent modes of variability of the alongshore coastal winds, covering event, seasonal and long-term scales;
nspicuous cycling between stratification and homogenisation observed in PCCC waters, which has key implications for the chemistry and biology of these waters;
asonal evolution of nitrite profiles in PCCC waters in relation to the stratification cycle;
dfield stoichiometry of the remineralisation of organic matter in Eastern North Atlantic Central Water (ENACW)—the water mass being transported by the PCCC;
paration of coastal (mesotrophic) from PCCC (oligotrophic) planktonic populations by a downwelling front along the shelf, which oscillates to and fro across the shelf as a function of coastal wind intensity and continental runoff; and
otosynthetic responses of the PCCC and coastal plankton populations to the changing stratification and light conditions from the onset to the cessation of the PCCC.