Long-wave Runup: Difference between revisions

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Revision as of 00:01, 14 January 2011

UNDER CONSTRUCTION

Overview

where $\eta$ is the water surface elevation, $\rho$ is the water density, $\rho _{a}$ is the air density, $g$ is the gravitational acceleration, $W$ is the wind speed, $h$ is the water depth, and $C$ is a constant of integration.

Initial Condition

Figure 1. Computed water surface elevation for the irregular domain with constant water depth.

Model Setup

A computational grid with constant water depth of 5 m and irregular boundaries is used in order to test the model performance. The computational grid has 60 columns and 70 rows and a constant resolution of 500 m.

Results

‎

Figure 2. Comparison of computed water surface elevation to the analytical solution for an irregular basin with constant depth.

References

Test Cases

Documentation Portal

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@@ Line 2: / Line 2: @@
 __NOTOC__
 <font color=red>'''UNDER  CONSTRUCTION'''</font>
-== Analytical Solution ==
+== Overview ==
+where <math>\eta</math> is the water surface elevation, <math>\rho</math> is the water density, <math>\rho_a</math> is the air density, <math>g</math> is the gravitational acceleration, <math>W</math> is the wind speed, <math>h</math> is the water depth, and <math>C</math> is a constant of integration.
-where <math>\eta</math> is the water surface elevation, <math>\rho</math> is the water density, <math>\rho_a</math> is the air density, <math>g</math> is the gravitational acceleration, <math>W</math> is the wind speed, <math>h</math> is the water depth, and <math>C</math> is a constant of integration.
+== Initial Condition ==
+[[Image:Long-wave_Runup_Initial_Water_Level.png|thumb|left|600px|   Figure 1. Computed water surface elevation for the irregular domain with  constant water depth.]]
+<br   style="clear:both" />
 == Model Setup ==
-A computational grid with constant water depth of 5 m and irregular boundaries is used in order to test the model performance. The computational grid has 60 columns and 70 rows and a constant resolution of 500 m.
+A computational grid with  constant water depth of 5 m and irregular boundaries is used in order to  test the model performance. The computational grid has 60 columns and  70 rows and a constant resolution of 500 m.
-== Initial Condition ==
-[[Image:Long-wave_Runup_Initial_Water_Level.jpg|thumb|left|600px|   Figure 1. Computed water surface elevation for the irregular domain with  constant water depth.]]
 == Results ==
-‎[[Image:Long-wave_Runup_Water_Level.jpg|thumb|none|600px| Figure 2. Comparison of computed water surface elevation to the analytical solution for an irregular basin with constant depth.]]
+‎[[Image:Long-wave_Runup_Water_Level.png|thumb|none|600px| Figure 2. Comparison of computed water surface elevation to the analytical solution for an irregular basin with constant depth.]]
 <br   style="clear:both" />
 == References ==