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Salinity stratification in a river-dominated estuary
Authors:William W Schroeder  Scott P Dinnel  William J Wiseman
Institution:1. Marine Science Program, The University of Alabama, P.O. Box 369, 36528, Dauphin Island, Alabama
2. Coastal Studies Institute, Louisiana State University, 70803, Baton Rouge, Louisiana
3. Coastal Studies Institute and Department of Geology and Geophysics, Louisiana State University, 70803, Baton Rouge, Louisiana
Abstract:Analysis of salinity data from Mobile Bay indicates that stratification-destratification events within this broad, shallow estuary are not uncommon. These events are related to the strength of the winds, through their influence on wave generation and subsequent bottom drag coefficient increases, and to the strength of river discharge. They do not appear to be due to the strength of tidal currents, as has been observed elsewhere. Furthermore, river flow appears to be the dominant control, the winds being important only in the absence of large freshwater discharges. The annual spring freshet can flush most of the salt from the bay. During other times of the year the relative strengths of river discharge and wind stress change the bay from highly stratified to nearly homogeneous and back on a variety of time scales ranging from daily to seasonal.
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