Required information Outside an inner, intense-activity circle of radius R, a tropical storm can be simulated by a polar coordinate velocity potential o (r, 0) = Uo R0, where Uo is the wind velocity at radius R. Take surface air density to be sea-level standard, p= 1.225 kg/m3. If, at R = 25 mi, the velocity is 105 mi/h and the pressure is 82000 Pa, calculate the velocity and pressure at r = 100 mi. The velocity is m/s. The pressure is Pa.

Required information Outside an inner, intense-activity circle of radius R, a tropical storm can be simulated by a polar coordinate velocity potential o (r, 0) = Uo R0, where Uo is the wind velocity at radius R. Take surface air density to be sea-level standard, p= 1.225 kg/m3. If, at R = 25 mi, the velocity is 105 mi/h and the pressure is 82000 Pa, calculate the velocity and pressure at r = 100 mi. The velocity is m/s. The pressure is Pa.

Principles of Heat Transfer (Activate Learning with these NEW titles from Engineering!)

8th Edition

ISBN:9781305387102

Author:Kreith, Frank; Manglik, Raj M.

Publisher:Kreith, Frank; Manglik, Raj M.

Chapter5: Analysis Of Convection Heat Transfer

Section: Chapter Questions

Problem 5.9P: When a sphere falls freely through a homogeneous fluid, it reaches a terminal velocity at which the...

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