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Petkovšek, Z.; Ribarič, M. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
The nonlinear equations for the two-dimensional small scale steady-state flow of a compressible fluid are put in a form appropriate for the treatment of streamlines with gentle slopes. For the limiting case when the slopes of the streamlines are negligibly small, these equations are solved numerically and the obtained results compared with the solutions of the linearized equations to determine the limits within which the linearization is permissible. Few numerical examples are given, to demonstrate the difference between solutions obtained by linearized and nonlinearized models of the atmosphere. It was found that the restriction that the total velocity of the wind be positive plays a decisive role in determining the maximum thickness of the air layer which is able to pass over a mountain of certain height.DOI: 10.1111/j.2153-3490.1965.tb00207.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • Doas, B. R., 1961, A mountain wave theory including tho effect nf wind and stability. Tellus, 13, pp. 305-319.
    • Doos, B. R., 1962, A theoretical analysis of the lee wave clouds observed by Tiros I. Ibid., 14, pp. 301-309.
    • QUENEYP,. et al., 1960, The airflow over mountains. W . M . O . Tech. Note, No. 34, Geneva.
    • SAWYERY,. S., 1959, The introduction of the effects of topography into methods of numerical forecasting. Quart. Y . R. Met. SOC.8,6, pp. 31-43.
    • SAWYERY,. S., 1960, Numerical calculations of the displacements of a stratified airstream crossing a ridge of small height. Ibid., 86, pp. 32G345.
    • KRISHN~~MURTIT,. N., 1964, The finite amplitude mountain wave problem with entropy as a vertical coordinate. Monthly Weather Review, 92, pp. 147- 160.
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