Abstract: tract

Abstract: In an attempt to understand the implications of Long's ?generalized dimensional analysis,? this method was applied to the problem of the wind distribution in the planetary boundary layer. The assumption was made that the ...

Abstract: In the study of wind profiles in the atmospheric surface layer it is important to distinguish between the speed of the mean vector wind |V|, which is equivalent to u WHEN THE x-axis is oriented in the downwind direction, ...

Abstract: Vertical gradients are usually calculated by a finite-difference approximation, where the level of interest is midway between the levels at which measurements are made. When this approach is used, considerable error may ...

Abstract: No Abstract Available.