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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Published in: | Atmospheric chemistry and physics Vol. 10; no. 5; pp. 2227 - 2236 |
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Main Authors: | , , , , |
Format: | Journal Article |
Language: | English |
Published: |
Copernicus Publications
03-03-2010
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Online Access: | Get full text |
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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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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 1680-7324 1680-7316 1680-7324 |
DOI: | 10.5194/acp-10-2227-2010 |