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A novel methodology to derive the average wind profile from the Navier-Stokesequations is presented. The development employs the Generalized IntegralTransform Technique (GITT), which combines series expansions with IntegralTransforms. The new approach provides a solution described in terms of thequantities that control the wind vector with height. Parameters, such asdivergence and vorticity, whose magnitudes represent sinoptic patterns arecontained in the semi-analytical solution. The results of this new methodapplied to the convective boundary layer are shown to agree with wind datameasured in Wangara experiment

A semi-analytical solution for the mean wind profile in the Atmospheric Boundary Layer: the convective case