Abstract
A method is given for the numerical solution of the barotropic vorticity equation over a limited area of the earth’s surface. The lack of a natural boundary calls for an investigation of the appropriate boundary conditions. These are determined by a heuristic argument and are shown to be sufficient in a special case. Approximate conditions necessary to insure the mathematical stability of the difference equation are derived. The results of a series of four 24-hour forecasts computed from actual data at the 500 mb level are presented, together with an interpretation and analysis. An attempt is made to determine the causes of the forecast errors. These are ascribed partly to the use of too large a space increment and partly to the effects of baroclinicity. The role of the latter is investigated in some detail by means of a simple baroclinic model.
1 On leave from Det Norske Meteorologiske Institut, Oslo, Norway.
2 This work was prepared under Contract N-6-ori-139 with the Office of Naval Research.
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© 1990 American Meteorological Society
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Charney, J.G., Fjörtoft, R., von Neumann, J. (1990). Numerical Integration of the Barotropic Vorticity Equation. In: Lindzen, R.S., Lorenz, E.N., Platzman, G.W. (eds) The Atmosphere — A Challenge. American Meteorological Society, Boston, MA. https://doi.org/10.1007/978-1-944970-35-2_15
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DOI: https://doi.org/10.1007/978-1-944970-35-2_15
Publisher Name: American Meteorological Society, Boston, MA
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