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Use the mass continuity equation to derive an expression for the vertical velocity at the top of a planetary boundary layer of fixed depth H3 in which the zonal wind is u(x)=U,cos(2tx/L). U. and L are constant with time and height in the boundary layer. There is no motion in the y direction and the surface is strictly horizontal. Neglect variations in density.

Use the mass continuity equation to derive an expression for the vertical velocity at the top of a planetary boundary layer of fixed depth H3 in which the zonal wind is u(x)=U,cos(2tx/L). U. and L are constant with time and height in the boundary layer. There is no motion in the y direction and the surface is strictly horizontal. Neglect variations in density.

Elements Of Electromagnetics
Elements Of Electromagnetics
7th Edition
ISBN:9780190698614
Author:Sadiku, Matthew N. O.
Publisher:Sadiku, Matthew N. O.
ChapterMA: Math Assessment
Section: Chapter Questions
Problem 1.1MA
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Use the mass continuity equation to derive an expression for the vertical velocity at the top of a planetary boundary layer of fixed depth HB in which the zonal wind is u(x)=U, cos(2xx/L). U. and L are constant with time and height in the boundary layer. There is no motion in the y direction and the surface is strictly horizontal. Neglect variations in density.
Transcribed Image Text:Use the mass continuity equation to derive an expression for the vertical velocity at the top of a planetary boundary layer of fixed depth HB in which the zonal wind is u(x)=U, cos(2xx/L). U. and L are constant with time and height in the boundary layer. There is no motion in the y direction and the surface is strictly horizontal. Neglect variations in density.
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