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Barotropic,subtidal exchange between Calcasieu Lake and the Gulf of Mexico
Authors:J. M. Lee  W. J. Wiseman  F. J. Kelly
Affiliation:1. Department of Marine Sciences, Louisiana State University, 70803, Baton Rouge, Louisiana
2. Department of Geology and Geophysics Coastal Studies Institute, Louisiana State University, 70803, Baton Rouge, Louisiana
3. Department of Environmental Engineering, Texas A & M University, 77843, College Station, Texas
Abstract:Long-term measurements of flow through Calcasieu Pass, Louisiana, are compared to water level variations within Calcasieu Lake, Louisiana. Except during periods of freshets driven by local rainfall, the exchange is shown to be predominantly barotropic. A simple wind-driven model accounts for the observed phase relations between wind, current, and water level.
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