Question: As illustrated below, a tornado can be approximated by a free vortex of strength for r > R c where R c is the radius
As illustrated below, a tornado can be approximated by a free vortex of strength for where is the radius of the core. Velocity measurements at points A and B indicate that and Determine the distance from point A to the center of the tornado. Why can the free vortex model not be used to approximate the tornado throughout the flow field? Hint: consider the velocity at the center of a free vortex and the actual velocity at the center of a tornado
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