Note
Recording current meter data from two study sites, 6 and 34 km off the central Texas Gulf coast are compared for a 36-day period in the spring of 1977. Nearshore motion over the mid and inner continental shelf exhibits many of the characteristics which support the concept of a coastal boundary layer lying within approximately 10 km of the coast. Cross-shelf variations in longshore and cross-shelf current components, and in the coherence between longshore motion and the longshore component of the wind-stress suggest that several distinctions exist between current patterns in inner and mid shelf waters.