Some Characteristic Features of the Large-Scale Disturbance in a Baroclinic Zonal Current
Author:
Affiliation:
1. Meteorological Research Institute
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1923/41/2/41_2_82/_pdf
Reference20 articles.
1. Aihara, M., 1959: Stability properties of large-scale baroclinic disturbances in a vertically and horizontally variable zonal current. Journ. Met. Soc. Japan, Ser. II, 37, 45-59.
2. Aihara, M., 1961: Time-dependent behaviours of parallel flows in a nondivergent barotropic atmosphere. Journ. Met. Soc. Japan, Ser. II, 39, 157-174.
3. Baer, F., 1961: The extended numerical integration of a simple barotropic model. Journ. Met., 18, 319-339.
4. Bryan, K., 1959: A numerical investigation of certain features of the general circulation. Tellus, 11, 163-173.
5. Charney, J. G., 1951: On baroclinic instability and the maintenance of the kinetic energy of the westerlies. Comp. Rend. d. Symposium sur la Circulation Generale des Oceans et de l'Atmossphere. Brux. aout, pp. 47-63.
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1. The influence of the time change of static stability and wind shear on baroclinic waves;Pure and Applied Geophysics PAGEOPH;1980-09
2. The developing circulation patterns on a β-plane obtained in the case of an initial basic flow varying sinusoidally with latitude;Archiv für Meteorologie, Geophysik und Bioklimatologie Serie A;1966-04
3. Some Remarks on the Treatment of Finite Amplitude Disturbances in the Baroclinic Atmosphere;Journal of the Meteorological Society of Japan. Ser. II;1966
4. Energy Cycle in the Lower Atmosphere;Journal of the Meteorological Society of Japan. Ser. II;1965
5. Growth of the Baroclinic Disturbance and Asymptotic Approach toward Finite Amplitude Steady State;Journal of the Meteorological Society of Japan. Ser. II;1964
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