Removing the Depth Dependence: Difference between revisions

From WikiWaves
Jump to navigationJump to search
mNo edit summary
No edit summary
Line 9: Line 9:
</math>
</math>


where <math>k</math> is the positive root of the [[Dispersion Equation]]
where <math>k</math> is the positive root of the [[Dispersion Relation for a Free Surface]]
then the problem reduces to [[Helmholtz's Equation]]
then the problem reduces to [[Helmholtz's Equation]]


Line 15: Line 15:


in the region not occupied by the scatterers.
in the region not occupied by the scatterers.
[[Category:Linear Water-Wave Theory]]

Revision as of 01:28, 2 June 2006

We are considering the Frequency Domain Problem for linear wave waves. If we have a problem in which the water depth is of constant depth [math]\displaystyle{ z=-d }[/math] (we are assuming the free surface is at [math]\displaystyle{ 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 Relation for a Free Surface 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.