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Smith, Phillip J. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
Energy budget equations applicable to any limited atmospheric region are developed employing the concept of available potential energy. These equations contain, in addition to the customary generation, conversion, and dissipation terms, expressions for the boundary fluxes. Utilizing Lorenz's definition of available potential energy, the energetics of the limited region are defined as the contribution that the region makes to the global energy budget. This allows one to examine energy processes in a limited region in terms of their relation to the energetics of the general circulation.DOI: 10.1111/j.2153-3490.1969.tb00432.x
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    • Dutton, J. A., and Johnson, D.R., 1967.TheTheory of Available Potential Energy and a Variational Approach to Atmospheric Energetics. Advances i n Ueophysics 12, New York, Academic Press, 333-436.
    • Holopainen, E. O., 1963. On the Dissipation of Kinetic Energy in the Atmosphere. Tellus 15, No. 1, 26-32.
    • Kung, E. C., 1966~K.inetic Energy Generationand Dissipation in the Large-scale Atmospheric Circulation. Monthly WeatherReview 94, No. 2,67-82.
    • Kung, E. C., 1966b. Large-scale Balance of Kinetic Energy in the Atmosphere. Monthly Weather Review 94, No. 11, 627-640.
    • Kung, E. C., 1967. Diurnal and Long-Term Variations of the Kinetic Energy Generation and Dissipation for a Five-Year Period. Monthly Weather Review 95, No. 9, 593-606.
    • Lorenz, E. N., 1955a. Available Potential Energy and the Maintenance of the General Circulation. Tellus 7, No. 2, 157-167.
    • Lorenz, E. N., 19556. Generation of Available Potential Energy and the Intensity of the General Circulation. Large Scale Synoptic Processes, University of California (Los Angeles), Department of Meteorology, Final Report, J. Bjerknes, Project Director.
    • Margules, M., 1903. Ober die Energie der St.iirme. Jahrb. Zentrahnst. Meterol. 1-26. (Translationby C. Abbe (1910) in Smithaonian Institute Miscellaneowr Collection 51, 553-595.)
    • Oort, A. H., 1964. On Estimates of the Atmospheric Energy Cycle. Monthly Weather Review 92, No. 11, 483-493.
    • Pfeffer, R. L., 1957. On the Physical Significance of Energy Transformation Functions. Studies of the Atmospheric General Circulation I I , Massachusetts Institute of Technology, Department of Meteorology, Final Report, General Circulation Project, V. P. Starr, Director.
    • Pfeffer, R. L., Mardon, D., Sterbenz, P., and Fowlis, W., 1966. A New Concept of Available Potential Energy. Report No. 66-1, Florida State University, Department of Meteorology.
    • van Mieghem, J., 1956. The Energy Available in the Atmosphere for Conversion into Kinetic Energy. Beitrage zur Physik der Atmosphare 29, 129-142.
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