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Turbulent diffusion in the lower atmosphere : A hybrid simulation study

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  • Shih, Chau
  • Karplus, W.J.

Abstract

The turbulent diffusion equation is solved by means of a hybrid simulation approach. The wind velocity profile and eddy diffusivities which appear in the general diffusion equation are assumed to be function of height only. The simulation technique to solve the general diffusion equation is first discussed. The method is then applied to solve the evaporation problem which is characterized by complicated explicit expressions of wind profile and eddy diffusivities.

Suggested Citation

  • Shih, Chau & Karplus, W.J., 1970. "Turbulent diffusion in the lower atmosphere : A hybrid simulation study," Mathematics and Computers in Simulation (MATCOM), Elsevier, vol. 12(3), pages 130-137.
    • Handle: RePEc:eee:matcom:v:12:y:1970:i:3:p:130-137
    DOI: 10.1016/S0378-4754(70)80011-8
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    Cited by:

    1. Shizgal, Bernie D. & Napier, Duncan G., 1996. "Nonequilibrium effects in reactive systems; the effect of reaction products and the validity of the Chapman-Enskog method," Physica A: Statistical Mechanics and its Applications, Elsevier, vol. 223(1), pages 50-86.
    2. Caussade, B. & Piquemal, J. & Zarcone, C., 1973. "Principes d'un calculateur hybride associant un calculateur numerique a un reseau de resistances," Mathematics and Computers in Simulation (MATCOM), Elsevier, vol. 15(2), pages 62-64.

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