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

A novel methodology to derive the average wind profile from the Navier-Stokes equations is presented. The development employs the Generalized Integral Transform Technique (GITT), which combines series expansions with Integral Transforms. The new approach provides a solution described in terms of the...

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Bibliographic Details
Published in:Atmospheric chemistry and physics Vol. 10; no. 5; pp. 2227 - 2236
Main Authors: Buligon, L., Degrazia, G. A., Acevedo, O. C., Szinvelski, C. R. P., Goulart, A. G. O.
Format: Journal Article
Language:English
Published: Copernicus Publications 03-03-2010
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Summary:A novel methodology to derive the average wind profile from the Navier-Stokes equations is presented. The development employs the Generalized Integral Transform Technique (GITT), which combines series expansions with Integral Transforms. The new approach provides a solution described in terms of the quantities that control the wind vector with height. Parameters, such as divergence and vorticity, whose magnitudes represent sinoptic patterns are contained in the semi-analytical solution. The results of this new method applied to the convective boundary layer are shown to agree with wind data measured in Wangara experiment.
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ISSN:1680-7324
1680-7316
1680-7324
DOI:10.5194/acp-10-2227-2010