Difference between revisions of "Template:Incident plane wave"

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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]