Difference between revisions of "Removing the Depth Dependence"
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<math> | <math> | ||
| − | \ | + | \Phi(x,y,z) = \cosh \big( k (z+d) \big) \phi(x,y) |
</math> | </math> | ||
| + | |||
| + | where <math>k</math> is the positive root of the [[Dispersion Equation]] | ||
| + | then the problem reduces to [[Helmholtz's Equation]] | ||
| + | |||
| + | <math>\nabla^2 \phi - k^2 = 0 </math> | ||
| + | |||
| + | in the region not occupied by the scatterers. | ||
Revision as of 11:09, 22 April 2006
If we have a problem in which the water depth is of constant depth [math]\displaystyle{ z=-d/math\gt (we are assuming the free surface is at \lt math\gt z=0 }[/math]) and all the scatters are also constant with respect to the depth then we can remove the depth dependence by assuming that the dependence on depth is given by
[math]\displaystyle{ \Phi(x,y,z) = \cosh \big( k (z+d) \big) \phi(x,y) }[/math]
where [math]\displaystyle{ k }[/math] is the positive root of the Dispersion Equation then the problem reduces to Helmholtz's Equation
[math]\displaystyle{ \nabla^2 \phi - k^2 = 0 }[/math]
in the region not occupied by the scatterers.
