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Tellus Volume 6, 1954 - Issue 2
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Original Articles

Prognostic Equations for the Mean Motions of Simple Fluid Systems and Their Relation to the Theory of Large Scale Atmospheric Turbulence

Philip Ducan ThompsonU.S. Air Force Geophysics Research Directorate, Cambridge
(Major)
Pages 150-164 | Received 15 Dec 1952, Published online: 15 Dec 2016

References

  • CHARNEY, J. G., and PHILLIPS, N. A., 1953: Numerical Integration of the Quasi-Geostrophic Equations for Barotropic and Simple Baroclinic Flows. J. Meteor., 10, pp. 71–99.
  • EADY, E. T., 1952: Note on Weather Computing and the So-Called 21/2-Dimensional Model. Tellus, 4, pp. 157–168.
  • ELIASSON, A., 1952: Simplified Models of the Atmosphere, Designed for the Purpose of Numerical Weather Prediction. Tellus, 4. pp. 145–157.
  • FJORTOFT, R., 1952: On a Numerical Method of Integrating the Barotropic Vorticity Equation. Tellus, 4, pp. 179–195.
  • SAWYER, J. S., and BUSHEY, F. H., 1953: A Baroclinic Model Atmosphere Suitable for Numerical Integradon. J. Meteor., 10, pp. 54–59.
  • THOMPSON, P. D., 1953: On the Theory of Large-Scale Disturbances in a Two-Dimensional Baroclinic Equivalent of the Atmosphere. Quart. Jour. R.M.S., 79, pp. 51–69.

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