By G. Fischer (auth.), G. Fischer (eds.)
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Extra info for Thermodynamical and Dynamical Structures of the Global Atmosphere
Introduction to the Theoretical Meteorology, New York: Holt, Rinehast and Winston 1959. Holmboc. , Gustin. : Dynamic Meteorology, New York: John Wiley, London: Chapman and Hall 1952. Holton. : An Introduction to Dynamic Meteorology. Vol. 23 in International Geophysics Series 1979. Hoskins. J.. : Large-ScaleDynamical processesin the Atmosphere, New York, London, Paris, San Diego. San Francisco. Sao Paula, Sydney, Tokyo, Toronto: Academic Press 1983. Lorenz. : The Nature and Theory of the General Circulation of the Atmosphere, Geneva: WMO 1969.
The second term on the right-hand side is frequently denoted as generation; to be positive it requires a positive correlation between temperature and heating deviations. 16) where (4-4,) is proportional to the mass in a vertical column. rn-‘1 . 5 Energy and angular momentum budgets 4’ is the “roughness” of the free surface and is a measure of available potential energy that can be converted into kinetic energy. s. 17) is a conservative quantity. 19) Becausethere is no generation of energy by internal processes,kinetic and potential energy will decreasein time in the presenceof dissipation.
Gill. : Atmosphere-OceanDynamics, New York, London, Paris, San Diego, San Francisco, S5o Paula, Sydney. Tokyo. Toronto: Academic Press 1982. Godske. L.. Bergeron. , Bjerkncs. : Dynamic Meteorology and Weather Forecasting, American Meteorological Society, Boston and Carnegy Institution of Washington 1957. Gordon. : Elcmcnts of Dynamic Meteorology, London: The English Universities Press 1962. Haltincr. J.. Martin. : Dynamical and Physical Meteorology, New York, London, Toronto: McGraw-Hill Book Comp.
Thermodynamical and Dynamical Structures of the Global Atmosphere by G. Fischer (auth.), G. Fischer (eds.)