b) A wind stress of 0.2 N m-2 blows along a narrow (no Coriolis force acting) freshwater channel 10 m deep and that is open ended and the water is initially stationary. After a time of 2000s, the current in the channel reaches a steady value throughout the channel and is then balanced only by the vertical component of the turbulent friction. Estimate; (i) the average current reached in the channel after a time of t=2000 s (ii) A value of Az, the vertical turbulent eddy viscosity coefficient

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Chapter5: Analysis Of Convection Heat Transfer
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Problem 5.29P: Air at 20C flows at 1 m/s between two parallel flat plates spaced 5 cm apart. Estimate the distance...
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(b) A wind stress of 0.2 N m-2 blows along a narrow (no Coriolis force acting) freshwater channel 10 m deep and that is open ended and the water is initially stationary. After a time of 2000s, the current in the channel reaches a steady value throughout the channel and is then balanced only by the vertical component of the turbulent friction. Estimate; (i) the average current reached in the channel after a time of t=2000 s (ii) A value of Az, the vertical turbulent eddy viscosity coefficient
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