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Lönnqvist, Olov (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
Methods now in common use for making prognostic charts to a large extent are based on time derivatives, while the numerical methods start from space derivatives. That is the fundamental difference between them. It is shown that the present methods give at times very good results, and that the degree of success varies with the weather situation, characterized e. g. by the average interdiurnal pressure change over the test area. Because of this variation it would be desirable that every test of a numerical method includes a comparison with results obtained at some forecasting center or, at least, with the results of pure extrapolation.DOI: 10.1111/j.2153-3490.1952.tb01004.x
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    • UOLINU,., and CHARNEJY., 1951: Numerical Tendency Computations from the Barotropic Vorticity Equation. 'Tellits 3, 4. pp. 248-257.
    • RIEHL, H., and, Collab., 1 9 ~ 1 : Forecodrig iti Middle Lntitudes. Chicago. Univ. of Chic., Dep. of Met. 168 pp.
    • SAWYERJ., S., and BUSHBYF.. H., 1951: Note on the Numerical Integration of the Equations of Meteorological Dynamics. Telliis 3, 3, pp. 201-203.
    • SCHERHACR,., 1948: h'ciie hfetlrodeti der Wctfcrwolysc tirid Wetterprogrtosc. Berlin-Gottingen-Heidelberg. Springer-Verlag. 424 pp.
    • STAFFMEMBERSU,niversity of Stockholm, 195': Preli, minary Report on the Prognostic Value of Uarotropic Models in the Forecasting of 500 rnb Height Changes. Telliis 4. I , pp. 21-30.
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