Semi-analytical solution of the steady three-dimensional advection-diffusion equation in the planetary boundary layer

We present a three-dimensional solution of the steady-state advection-diffusion equation considering a vertically inhomogeneous planetary boundary layer (PBL). We reach this goal applying the generalized integral transform technique (GITT), a hybrid method that had solved a wide class of direct and...

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Bibliographic Details
Published inAtmospheric environment (1994) Vol. 40; no. 29; pp. 5659 - 5669
Main Authors Costa, C.P., Vilhena, M.T., Moreira, D.M., Tirabassi, T.
Format Journal Article
LanguageEnglish
Published Oxford Elsevier Ltd 01.09.2006
Elsevier Science
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Summary:We present a three-dimensional solution of the steady-state advection-diffusion equation considering a vertically inhomogeneous planetary boundary layer (PBL). We reach this goal applying the generalized integral transform technique (GITT), a hybrid method that had solved a wide class of direct and inverse problems mainly in the area of heat transfer and fluid mechanics. The transformed problem is solved by the advection-diffusion multilayer model (ADMM) method, a semi-analytical solution based on a discretization of the PBL in sub-layers where the advection-diffusion equation is solved by the Laplace transform technique. Numerical simulations are presented and the performances of the solution are compared against field experiments data.
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ISSN:1352-2310
1873-2844
DOI:10.1016/j.atmosenv.2006.04.054