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Estoque, Mariano A. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
The vertical and radial motions associated with a given tangential velocity and temperature distribution corresponding to a tropical cyclone are calculated using a diagnostic equation. The equation is derived by introducing the hydrostatic and gradient wind approximations systematically into the meteorological equations. The computed circulation pattern appears to reproduce most of the important characteristics of a mature cyclone such as the eye and the eyewall. The results also show that the sinking motion in the eye is thermally controlled.DOI: 10.1111/j.2153-3490.1962.tb01352.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • ELIASSENA,., 1952: Slow thermally or frictionally controlled meridional circulations in a circular vortex. Astrophysica Norvegica, 6, no. 2.
    • ELIASSEAN.,, 1 9 5 9 On the formation of fronts in the atmosphere. The Rossby Memorial Volume, Rockefeller Institute Press, N.Y.
    • LAVOIER,. L., 1956: An evaluation of radar results from hurricane research flights of 1955. (Unpublished M.S. degree thesis, Florida State University, 26 pp.)
    • KRISHNAMURTI.,N., 1961: On the vertical velocity field in a steady symmetric hurricane. Tellus, 13, pp. 171-180.
    • Kuo, H. L., 1959: Dynamics of convective vortices and eye formation. The Rossby Memorial Volume, Rockefeller Institute Press, N.Y.
    • PEDERSENK,., 1961: On the vertical circulation produced by release of latent heat i n a static and quasi-geostrophicatmosphere. Department of Meteorology, Univ. of Chicago, 12 pp.
    • RIEHL,H. and J. MALKUS, 1961: Some aspects of Hurricane Daisy, 1958. Tellus, 13, pp. 181-213.
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