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A tornado is a three-dimensional wind field that can be modeled as a velocity field. In this project we look at a two-dimensional slice of a vortex and use an Oseen vortex velocity field to model a tornado.
In rectangular coordinates, an Oseen velocity field is given by v=(Vmax
We place the center of the tornado at origin, where \mathbf{v} is undefined. Then \mathbf{v} gives the velocity of the wind at any other location within the vortex.
A fluid, like the air in a tornado, is considered to be incompressible if the divergence of its velocity field, {div}\mathbf{v }, equals 0. When a fluid is incompressible, it is possible to find a function, \psi ( x,y) , called a stream function. The level curves of a stream function are called stream lines. These are the curves along which particles of fluid would flow. (You may have seen examples of stream lines such as air moving around a car in a wind tunnel.) The stream function, \psi ( x,y) , for a velocity field, \mathbf{v}=h( x,y) \,\mathbf{i}+g( x,y) \,\mathbf{j}, where h and g are functions of x and y, satisfies \dfrac{\partial \psi }{\partial y}=h( x,y) \quad\hbox{and}\quad \dfrac{\partial \psi }{\partial x}=-g( x,y)
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