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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Main Authors: L. Buligon, G. A. Degrazia, O. C. Acevedo, C. R. P. Szinvelski, A. G. O. Goulart
Format: Article
Language:English
Published: Copernicus Publications 2010-03-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/10/2227/2010/acp-10-2227-2010.pdf
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author L. Buligon
G. A. Degrazia
O. C. Acevedo
C. R. P. Szinvelski
A. G. O. Goulart
author_facet L. Buligon
G. A. Degrazia
O. C. Acevedo
C. R. P. Szinvelski
A. G. O. Goulart
author_sort L. Buligon
collection DOAJ
description 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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spelling doaj.art-28c0679ee44e48999a6ad4a36a138b472022-12-21T19:51:07ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242010-03-0110522272236A semi-analytical solution for the mean wind profile in the Atmospheric Boundary Layer: the convective caseL. BuligonG. A. DegraziaO. C. AcevedoC. R. P. SzinvelskiA. G. O. GoulartA 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.http://www.atmos-chem-phys.net/10/2227/2010/acp-10-2227-2010.pdf
spellingShingle L. Buligon
G. A. Degrazia
O. C. Acevedo
C. R. P. Szinvelski
A. G. O. Goulart
A semi-analytical solution for the mean wind profile in the Atmospheric Boundary Layer: the convective case
Atmospheric Chemistry and Physics
title A semi-analytical solution for the mean wind profile in the Atmospheric Boundary Layer: the convective case
title_full A semi-analytical solution for the mean wind profile in the Atmospheric Boundary Layer: the convective case
title_fullStr A semi-analytical solution for the mean wind profile in the Atmospheric Boundary Layer: the convective case
title_full_unstemmed A semi-analytical solution for the mean wind profile in the Atmospheric Boundary Layer: the convective case
title_short A semi-analytical solution for the mean wind profile in the Atmospheric Boundary Layer: the convective case
title_sort semi analytical solution for the mean wind profile in the atmospheric boundary layer the convective case
url http://www.atmos-chem-phys.net/10/2227/2010/acp-10-2227-2010.pdf
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