Three-dimensional Treatments of Equations of Motion without Using the Geostrophic Approximation
Author:
Affiliation:
1. Geophsical Institute, Tokyo University
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1923/35/1/35_1_1/_pdf
Reference14 articles.
1. 1. Bolin, B. (1955): Numerical forecasting with the barotropic model. Tellus, 7, pp. 27-49.
2. 2. Bolin, B. (1956): An improved barotropic model and some aspects of using the balance equation for three-dimensional flow. Tellus, 8, pp. 61-75.
3. 3. Charney; J. H. (1948): On the scale of atmospheric motions. Geophys. Publ., 17, No. 2, pp. 1-17.
4. 4. Charney, J. H. (1955): The use of the primitive equations of motion in numerical prediction. Tellus, 7, pp. 2126.
5. 5. Eady, E. T. (1949): Long waves and cyclone waves, Tellus, 1, pp. 33-52.
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1. A Note on Geostrophic Adjustment and Gravity Wave in the Atmosphere;Journal of the Meteorological Society of Japan. Ser. II;1961
2. A Study of the Stationary Meteorological Fields of the Large Scale;Journal of the Meteorological Society of Japan. Ser. II;1959
3. Stability Properties of Large-scale Baroclinic Disturbances in a Vertically and Horizontally Variable Zonal Current;Journal of the Meteorological Society of Japan. Ser. II;1959
4. Numerical Analysis of Wind and its Application to the Numerical Weather Forecasting (Part 1);Journal of the Meteorological Society of Japan. Ser. II;1958
5. Equations of Motion for Small Scale Disturbances;Journal of the Meteorological Society of Japan. Ser. II;1957
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