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Original Articles

An Improved Barotropic Model and some Aspects of Using the Balance Equation for Three-dimensional Flow

Pages 61-75 | Received 11 Nov 1955, Accepted 24 Jan 1956, Published online: 15 Dec 2016

References

  • BERGGREN, R., BOLIN, B., ROSSEY, C.-G., 1949: An aerological study of zonal motion, its perturbations and break-down. Tellus, 1, 2, PP. 54–37.
  • BOLIN, B., 1953: The adjustment of a non-balanced velocity field towards geostrophic equilibrium in a stratified fluid. Tellus, 5, pp. 373–385.
  • BOLIN, B., 1955: Numerical forecasting with the baro-tropic model. Tellus, 7, PP. 27–49.
  • CHARNEY, J., 190: On the scale of atmospheric motions. Geofys. Publ. 27, 2, 17 pp.
  • CHARNEY, J., 1955: The use of the primitive equations of motion in numerical forecasting. Tellus, 7, pp. 22–26.
  • CHARNEY, J., ELIASSEN, A., 1949: A numerical method for predicting perturbations in the middle latitude westerlies. Tellus, 1, 2, pp. 38–54.
  • ROSSBY, C.-G., 1945: On the propagation of frequencies and energy in certain types of oceanographic and atmospheric waves. J. of Meteorology, 2, pp. 187–204.
  • THOMPSON, P. D., 1955 : A theory of large-scale dis-turbances in non-geostrophic flow. Report Joint Numerical Weather Prediction Unit, Washington, D.C.
  • YEH, T. C., 1949: On energy dispersion in the atmosphere. J. of Meteorology, 6, pp. 1–16.