![]() ![]() Except for the 5 m depth site A, where turbulent friction dominates the flow, the depth-averaged flow approximately follows the isobaths provided that the local radius of curvature of the isobaths is 5 km or larger. (i) Apart from the frictional surface and bottom boundary layers the flow is approximately barotropic for all seasons of the year. Analysis of these observations and their dynamics on subinertial and seasonal time scales led to the following conclusions. Eulerian acoustic Doppler current profiler measurements on this narrowing shelf, the first multiyear in situ measurements in this region, have been obtained at K-Tower, an Air Force navigational tower in 19 m of water about 33 km south of the Big Bend coast, at 5 m and 10 m depth along a section perpendicular to the coast from K-Tower, and in 19 m of water off the Florida peninsula about 45 km south of K-Tower. The northern part of the West Florida Shelf (WFS) bends sharply to form Florida's Big Bend coast.
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