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- W2730134921 endingPage "1996" @default.
- W2730134921 startingPage "1994" @default.
- W2730134921 abstract "Estuarine circulation are driven by the actions of tide, wind, and density gradients associated with saline ocean water and fresh riverine water, and are also influenced by the complex geometry and bathymetry of the estuaries in the U.S. (e.g.,Tampa Bay and Chesapeake Bay) are generally quite shallow except within the navigation channels. In general, there is significant vertical and horizontal stratification in the channel. In the shallow shoals, there is often significant horizontal stratification in the channel. In the shallow shoals, there is often significant horizontal stratification, although it is generally well mixed in the vertical direction. Proper parameterization of turbulent mixing in the vertical and horizontal directions is essential to the accurate simulation of mean circulation and transport, and has been a challenge for estuarine modeling in the past decade." @default.
- W2730134921 created "2017-07-14" @default.
- W2730134921 creator A5047786472 @default.
- W2730134921 date "1993-01-01" @default.
- W2730134921 modified "2023-09-28" @default.
- W2730134921 title "Parameterization of Turbulence for Three-Dimensional Circulation Modeling" @default.
- W2730134921 hasPublicationYear "1993" @default.
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