A semi-analytical solution for the mean wind profile in the Atmospheric Boundary Layer: the convective case 1Universidade Federal de Santa Maria, Departamento de Física, Santa Maria, RS, Brazil
2Universidade Federal do Pampa/UFSM, Centro de Ciências Exatas e Tecnológicas, Bagé, RS, Brazil
3Centro de Educação Superior do Alto Vale do Itajaí, UDESC/CEAVI, Ibirama, SC, Brazil
Received: 26 Jun 2009 – Published in Atmos. Chem. Phys. Discuss.: 23 Sep 2009 Abstract. 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.
Revised: 28 Dec 2009 – Accepted: 31 Jan 2010 – Published: 03 Mar 2010
Citation: Buligon, L., Degrazia, G. A., Acevedo, O. C., Szinvelski, C. R. P., and Goulart, A. G. O.: A semi-analytical solution for the mean wind profile in the Atmospheric Boundary Layer: the convective case, Atmos. Chem. Phys., 10, 2227-2236, doi:10.5194/acp-10-2227-2010, 2010.