Semi-analytical solution of the steady three-dimensional advection-diffusion equation in the planetari boundary layer (Articolo in rivista)

Type
Label
  • Semi-analytical solution of the steady three-dimensional advection-diffusion equation in the planetari boundary layer (Articolo in rivista) (literal)
Anno
  • 2006-01-01T00:00:00+01:00 (literal)
Alternative label
  • COSTA, C.P., VILHENA, M.T., MOREIRA, D. M. e TIRABASSI, T. (2006)
    Semi-analytical solution of the steady three-dimensional advection-diffusion equation in the planetari boundary layer
    in Atmospheric environment (1994)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • COSTA, C.P., VILHENA, M.T., MOREIRA, D. M. e TIRABASSI, T. (literal)
Pagina inizio
  • 5659 (literal)
Pagina fine
  • 5669 (literal)
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  • 40 (literal)
Rivista
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  • 10 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Univ Fed Rio Grande Sul, PROMEC, BR-90050170 Porto Alegre, RS, Brazil Univ Fed Rio Grande Sul, PROMEC, BR-90050170 Porto Alegre, RS, Brazil Univ Fed Rio Grande Sul, PPGMAP, Inst Math, BR-90050170 Porto Alegre, RS, Brazil CNR, ISAC, Bologna, Italy (literal)
Titolo
  • Semi-analytical solution of the steady three-dimensional advection-diffusion equation in the planetari boundary layer (literal)
Abstract
  • 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 GITT (Generalized Integral Transform Technique), 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 ADMM (Advection-Diffusion Multilayer Model) 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. (literal)
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