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

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

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134 A <strong>Semi</strong>-<strong>Implicit</strong>, <strong>Three</strong>-<strong>Dimensional</strong> <strong>Model</strong> <strong>for</strong> <strong>Estuarine</strong> Circulation<br />

u VELOCITY COMPONENT,<br />

IN CENTIMETERS PER SECOND<br />

WATER SURFACE ELEVATION,<br />

IN CENTIMETERS<br />

w VELOCITY COMPONENT,<br />

IN CENTIMETERS PER SECOND<br />

30<br />

20<br />

10<br />

0<br />

-10<br />

-20<br />

-30<br />

30<br />

20<br />

10<br />

0<br />

-10<br />

-20<br />

-30<br />

0.015<br />

0.010<br />

0.005<br />

0<br />

-0.005<br />

-0.010<br />

Node i = 13, j = 5<br />

Node i = 2, j = 5<br />

Node i = 2, j = 5, k = 3<br />

Computed Analytical<br />

-0.015<br />

0 5<br />

1 0<br />

1 5<br />

2 0<br />

TIME, IN HOURS<br />

Figure 5.25. Twenty-hour time history of computed and analytical solutions <strong>for</strong> the seiching of an ideal fluid.<br />

The numerical solution is computed using the 3-dimensional semi-implicit leapfrog scheme and a time step<br />

of 45 seconds.

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