The Linear Response of a Global Atmosphere to Mobile Heating
Author:
Affiliation:
1. Meteorological Research Institute
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/75/4/75_4_867/_pdf
Reference11 articles.
1. Chalikov, D. V., A. S. Monin, A. S. Safray, B. G. Turikov and S. S. Zilitinkevich, 1975: Numerical simulation of the general circulation of the Cytherean lower atmosphere. ICARUS, 26, 178-208.
2. Del Genio, A. D., W. Zhou and T. P. Eichler, 1993: Equatorial superrotation in a slowly rotating GCM: implications for Titan and Venus. ICARUS, 101, 1-17.
3. Gill, A. E., 1980: Some simple solutions for heat-induced tropical circulation. Quart. J. Roy. Meteor. Soc., 106, 447-462.
4. Hoskins, B. J. and D. J. Karoly, 1982: the steady linear response of a spherical atmosphere to thermal and orographic forcing. J. Atoms. Sci., 38, 1179-1196.
5. Kasahara, A., 1984: The linear response of a stratified global atmosphere to tropical thermal forcing. J. Atmos. Sci., 41, 2217-2237.
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1. The Thermal Phase Curve Offset on Tidally and Nontidally Locked Exoplanets: A Shallow Water Model;The Astrophysical Journal;2017-06-20
2. Thermally Driven Tropical Circulations under Rayleigh Friction and Newtonian Cooling: Analytic Solutions*;Journal of the Atmospheric Sciences;2001-04
3. The Nonlinear Response of a Slowly-Rotating Atmosphere to Mobile Heating : Numerical Experiments of Relevance to the Venusian Atmosphere;Journal of the Meteorological Society of Japan. Ser. II;1998
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