Difference between revisions of "Template:Standard linear problem notation"

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We denote <math>\mathbf{r}=(x,y)</math> as the horizontal coordinate in two or three dimensions
 
We denote <math>\mathbf{r}=(x,y)</math> as the horizontal coordinate in two or three dimensions
 
respectively and the cartesian system we denote by <math>\mathbf{x}</math>.  
 
respectively and the cartesian system we denote by <math>\mathbf{x}</math>.  
We assume that the bottom surface is of constant depth but [[Variable Bottom Topography]]
+
We assume that the bottom surface is of constant depth <math>h</math>.
can easily be included.
 

Revision as of 07:30, 24 August 2008

We assume small amplitude so that we can linearise all the equations. We also assume that Frequency Domain Problem with frequency [math]\displaystyle{ \omega }[/math] The water motion is represented by a velocity potential which is denoted by [math]\displaystyle{ \phi }[/math]. The coordinate system is the standard Cartesian coordinate system with the [math]\displaystyle{ z }[/math] axis pointing vertically up. The water surface is at [math]\displaystyle{ z=0 }[/math] and the region of interest is [math]\displaystyle{ -h\lt z\lt 0 }[/math]. There is a body which occupies the region [math]\displaystyle{ \Omega }[/math] and we denoted the wetted surface of the body by [math]\displaystyle{ \partial\Omega }[/math] We denote [math]\displaystyle{ \mathbf{r}=(x,y) }[/math] as the horizontal coordinate in two or three dimensions respectively and the cartesian system we denote by [math]\displaystyle{ \mathbf{x} }[/math]. We assume that the bottom surface is of constant depth [math]\displaystyle{ h }[/math].