A Semi-Implicit, Three-Dimensional Model for Estuarine ... - USGS

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110 A Semi-Implicit, Three-Dimensional Model for Estuarine Circulation ROOT MEAN SQUARE ERROR, IN PERCENT AMPLITUDE ERROR, IN PERCENT 10 9 8 7 6 5 4 3 2 1 0 −1 30 25 20 15 10 5 0 −5 −10 −15 Leapfrog Leapfrog-trapezoidal, 1 iteration Leapfrog-trapezoidal, 4 iterations 0 5 10 15 20 Δ t, IN MINUTES Figure 5.10. Error measures using the three-level semi-implicit scheme on the hydrograph test problem for different values of the computational time interval (Δt). Δx = 2,000 feet for all simulations. Δx is the size of the computational space interval.
PHASE ERROR, IN PERCENT MASS PRESERVATION ERROR, IN PERCENT 8 6 4 2 0 −2 5 4 3 2 1 0 −1 Leapfrog Leapfrog-trapezoidal, 1 iteration Leapfrog-trapezoidal, 4 iterations −2 0 5 10 15 20 Figure 5.10. Continued. Δ t, IN MINUTES 5. Numerical Experiments 111
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In cooperation with the Interagency
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U.S. Department of the Interior Dir
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vi 4.2 Semi-Implicit One-Dimensiona
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viii Figure 5.6. Graph showing solu
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x Tables Table 2.1. Dimensionless n
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2 A Semi-Implicit, Three-Dimensiona
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2.4.1.2 Dynamic Surface Condition 2
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Water surface Water surface Level p
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h 1 h 2 h 3 h 4 h 5 h 6 z 1 ⁄ 2 z
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A Semi-Implicit, Three-Dimensional Model for Estuarine ... - USGS

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