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Bring, A.; Charasch, E. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
The result of a test with two simple non-geostrophic barotropic models are discussed. One of these models is based on ideas presented in a previous article (Charash 1957). The forecasts obtained are found to differ significantly from forecasts obtained with the quasi-geostrophic model. Both non-geostrophic models appear to be free from one major weakness of the non-geostrophic model, i.e. the hypertrophy of anticyclones. It is suggested that the disappointing forecasting performance of baroclinic models hitherto to a considerable degree springs from a similar weakness as exposed here in the quasi-geostrophic barotropic model.DOI: 10.1111/j.2153-3490.1958.tb01988.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • A N D E. C H A R A S C H BERGTHORSSPO., ND,OOs, B., 195s: Numerical Weather Map Analysis, Tellus, 7, pp. 329-340.
    • ~ w~., 1~9s6:, iff^^^^^^^ in ~
    • arising from iff^^^^^^^. in Analyses, Tellus, 8, pp. 351-3 56.
    • B O W B., 1955: Numerical Forecasting with the Barotropic Model. Tellus, 7, pp. 27-49.
    • BOLIN,B., 1956: An Improved Barotropic Model and some Aspects of Using the Balance Equation for Three Dimensional Flow. Tellus 8, pp. 1-15.
    • ~ F~~~~~~~~~ CHAR~ASCHE.,, 19~57: Note i on nume~rical predi~ction of l intensity changes of disturbances with the aid of the quasi-geostrophic barotropic model. Tellus 10.
    • PP, 99-98.
    • sCHUMAF.,N1,955: A method for solvingthe balance equation. Technical Memorandum 6, Joint Numerical Weather Prediction Unit.
  • No related research data.
  • Discovered through pilot similarity algorithms. Send us your feedback.

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