Simulation of Water Levels Sample Clauses

Simulation of Water Levels. In order to analyze tidal propagation, a series of 3-hour interval data was extracted from the 30 days of recorded simulation results. The water level on the 501st hour at S1 was selected as a beginning frame for the tidal cycle, slack before flood (Figure 2-8). Figures 2-9a and 2-9b show salinity distribution at 3-hour intervals starting at Hour 501. Barataria Basin is morphologically separated from the Gulf of Mexico by the several islands that block tidal energy from propagating into the bay. Figures 2-9a and 2-9b suggest that the tidal regime within the basin can be divided into four different regions: (1) the Gulf of Mexico, (2) Barataria Bay and Caminada Bay regions, (3) Little Lake and Barataria Waterway regions, and (4) the upper basin regions of Lac des Allemands and Lake Salvador. The separations are characterized by a chain of islands, narrow canals and bayous, and the Gulf Intracoastal Waterway. During the period shown in Figures 2-9a and 2-9b, the tidal range is roughly 40 cm near the mouth of the bay. The tidal amplitudes decrease as tides propagate into the upstream regions. There are some discontinuities at the transitions between Barataria Bay and Barataria Waterway, Little (a) Mississi ppi River Discharge at Venice Water Level (meter) 1.5 0.5 0 1000 2000 3000 4000 5000 6000 7000 8000
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