Template:Incident plane wave: Difference between revisions

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The equation is subject to some radiation conditions at infinity. We usually assume that
The equation is subject to some radiation conditions at infinity. We assume the following.
there is an incident wave <math>\phi^{\mathrm{{In}}}\,</math> 
{{incident plane wave 2d definition}}
is a plane wave travelling in the <math>x</math> direction
<center><math>
\phi^{\mathrm{{In}}}({r},z)=Ae^{k_0 x}\frac{\cos k_0(z+h)}{\cos k_0 h}
</math></center>
where <math>A</math> is the wave amplitude and <math>k_0</math> is
the positive imaginary solution of the [[Dispersion Relation for a Free Surface]].
We also have to apply the [[Sommerfeld Radiation Condition]] as <math>\left|\mathbf{r}\right|\rightarrow
\infty</math>.

Latest revision as of 03:15, 26 November 2009

The equation is subject to some radiation conditions at infinity. We assume the following. [math]\displaystyle{ \phi^{\mathrm{I}}\, }[/math] is a plane wave travelling in the [math]\displaystyle{ x }[/math] direction,

[math]\displaystyle{ \phi^{\mathrm{I}}(x,z)=A \phi_0(z) e^{\mathrm{i} k x} \, }[/math]

where [math]\displaystyle{ A }[/math] is the wave amplitude (in potential) [math]\displaystyle{ \mathrm{i} k }[/math] is the positive imaginary solution of the Dispersion Relation for a Free Surface (note we are assuming that the time dependence is of the form [math]\displaystyle{ \exp(-\mathrm{i}\omega t) }[/math]) and

[math]\displaystyle{ \phi_0(z) =\frac{\cosh k(z+h)}{\cosh k h} }[/math]