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Hassanein, S. A. M. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
A solution of the vorticity equation is obtained for a wave pattern changing with time. It is shown that such a wave pattern is necessarily associated with ridge and trough lines which do not run in the south-north direction.DOI: 10.1111/j.2153-3490.1949.tb01275.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • HAURWITZB, ., 1940: The motion of atmospheric disturbances. I. Mar. Res., 3, I,pp. 35-50.
    • Kuo, HSIAO-LAN1,949: Dynamic instability of two dimensional non divergent flow. J . Mefeor., 6, 2, pp. 105-122.
    • MACHTAL,., 1949: Dynamic characteristics of a tilted trough model. J. Meteor., 6, 4, pp. 261-265.
    • M I E ~ H EJM. ,VAN, 1949: Production et redistribution de la quantite dc inouvemcnt et de I'inergie cinCtique dans I'atniosph6re. Application la circulation atmosphCrique gfnirale. J . Sc. de In MJfLor., I, 2 , PP. 53-47.
    • ROSSBY,C. G.,1939: Relation between varations in the intensity of the zonal circulation of the atmosphere and the displacements of the semi-permanent centres of action. J . Mar. Res., 2, I , pp. 38-55,
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