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A fine-resolution primitive equationnumerical model is constructed for the Iberian continental shelf and sloperegion, with open boundaries to the north, south and west. The model is forcedby climatological wind fields and relaxed at the surface to climatologicaltemperature and salinity fields. A series of numerical experiments is conductedto investigate the influence of the open boundary conditions. The numericalresults include coastal upwelling in summer and a poleward current in winter.The effects of advection of Mediterranean Water and eastern North AtlanticCentral Water feature in the circulation. Qualitative comparisons are made withobservations

Sensitivity to open boundary forcing in a fine-resolution model of the Iberian shelf-slope region