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Charasch, Elishu (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
It is shown by a simple analysis that the introduction of a small but systematic error in the evaluation of vorticity causes a significant aberration in the conversion process between disturbance and basic flow kinetic energy in barotropic motion. The neglect of the variation of the coriolis parameter in the geostrophic vorticity is shown to be responsible for large errors in the prediction of the intensity changes taking place in a barotropic model.DOI: 10.1111/j.2153-3490.1958.tb01989.x
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    • BRING, A., CHARASCH, E., 1957: An experiment in numerical prediction with two non-geostrophic barotropic models. Tel/us, 9, pp. 88-94.
    • GATES, W. LAWRENCE, POCINKI, 1. S., JENKINS, C. F., 1955 : Results of numerical forecasting with the barotropic and thermotropic atmospheric models. Geophys. Research Papers, 46.
    • HASSANEIN, S. A. M., 1949: A wave pattern changing with time as a solution of the vorticity equation for non-divergent motion. Tel/us, I, 4, pp. 58-60.
    • Kuo, H. 1., 1951: A note on the kinetic energy balance of the zonal wind systems. Tel/us, 3 pp. 205-207.
    • - 1949: Dynamic instability of two-dimensional nondivergent flow in a barotropic atmosphere. Journal of Meteorology, 6, pp. 356-358.
    • MACHTA, 1., 1949: Dynamic characteristics of a tilted trough model. Journal of Meteorology, 6, pp. 261­
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