Abstract
The relationship between anchovy (Engraulis encrasicolus) recruitment in the Bay of Biscay and environmental variables during their planktonic phase (March to July) was investigated from 1986 to 1997. Meteorological variables (wind and temperature) are forcing effects on the sea, but they are not thought to be processes that govern larval survival directly. Food‐web dynamics are believed to be more closely linked to larval survival and are related to the physical vertical water column structure. Therefore, we used a three‐dimensional (3D) hydrodynamic model to characterize three major physical mesoscale processes affecting vertical structure in south‐east Biscay: stratification, upwelling and river plume extent. Indices were estimated from the model outputs to characterize and quantify the space/time evolution of these structures during the period March to July. A multiple linear regression analysis was then used to analyse hierarchy in the explanatory power of the physical indices. Coastal upwelling and shelf stratification breakdown indices were the most significant explanatory variables, with positive and negative effect on recruitment, respectively. A model with these two indices explains 75% of the recruitment variability of anchovy observed in the period 1987–96.
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