Abstract

In the atmospheric boundary layer there are horizontal pressure gradient and Coriolis force to the velocity distribution signify that the horizontal component of the velocity in the boundary layer turns left right with increasing height in the Southern Northern Hemisphere downward upward motion occurs on the windward lee side of the mountain and downward upward motion also occurs on the slope to the right left of the geostrophic wind in the Northern Hemisphere whereas in the Southern Hemisphere upward downward motion occurs on the slope to the left right of the geostrophic wind Using Navier-Stokes equations for threedimensional stationary flows hydrostatic and continuity equations the effects of first order reactant of Coriolis force and dust particles for small Reynolds number in the atmospheric boundary layer over territory is obtained