References
- Arakawa, A. and Schubert, W. H. 1974. Interaction of a cumulus cloud ensemble with the large-scale environment, Part I. J. Atmos. Sc i. 31, 674–701.
- Arpe, K., Brankovic, C., Oriol, E. and Speth, P. 1986. Variability in time and space of energetics from a long series of atmospheric data produced by ECMWF. Beitr. Phys. Atmos. 59, 321–355.
- Batchelor, G. K. 1967. An introduction to fluid dynamics. Cambridge University Press, 615 pp.
- Bernhardt, K. 1979. Zur Frage der Gfiltigkeit der Reynoldsschen Postulate. Zeitschr. Meteorol. 30, 361–368.
- Boer, G. J. 1975. Zonal and eddy forms of the available potential energy equations in pressure coordinates. Tellus 27, 433–443.
- Boer, G. J. 1976. Reply to J. Egger. Tellus 28, 379-380.
- Cotton, W. and Anthes, R. A. 1989. Storm and cloud dynamics, vol. 44 of Int. Geophys. Ser. Academic Press, 883 pp.
- Dutton, J. A. and Johnson, D. R. 1967. The theory of available potential energy and a variational approach to atmospheric energetics. Adv. Geophys. 12, 333–437.
- Emanuel, K. A. 1994. Atmospheric convection. Oxford University Press, 580 pp.
- Falk, G. and Ruppel, W. 1976. Energie und Entropie. Eine Einfiihrung in die Thermodynamik. Springer, 408 pp.
- Glansdorff, P. and Prigogine, I. 1971. Thermodynamic theory of structure, stability and fluctuations. Wiley, 306 pp.
- Haimberger, L. and Hantel, M. 2000. Implementing con-vection into Lorenz’s global cycle, Part II: A new estimate of the conversion rate into kinetic energy. Tellus 52A, 75–92.
- Herbert, F. 1975. Irreversible processes in the atmo-sphere - Part 3 (Phenomenological theory of micro-turbulent systems). Beitr. Phys. Atmos. 48, 1–29.
- Hesselberg, T. 1926. Die Gesetze der ausgeglichenen atmosphdrischen Bewegungen. Beitr. Phys. frei Atmos. 12, 141–160.
- Kraus, E. B. and Businger, J. A. 1994. Atmosphere-ocean interaction. Oxford University Press, 362 pp.
- Kucharski, F. 1997. On the concept of exergy and available potential energy. Quart. J. Roy. Meteor. Soc. 123, 2141–2156.
- Leonard, A. 1974. Energy cascade in large-eddy simula-tions of turbulent fluid flows. In: Turbulent diffusion in environmental pollution (eds. Frenkiel, F. and Munn, R.), vol. 18A of Adv. Geophys., pp. 237–248. Academic Press.
- Lorenz, E. N. 1955. Available potential energy and the maintenance of the general circulation. Tellus 7, 157–167.
- Lorenz, E. N. 1967. The nature and theory of the general circulation of the atmosphere, vol. 218.TP.115. WMO, 161 pp.
- Margules, M. 1903. Ober die Energie der Stfirme. Jahrb. k. k. Zent.-Anst. far Meteorol. und Erd magnet. 48, 1–26.
- Newell, R. E., Vincent, D. G., Dopplick, T. G., Ferrfizza, D. and Kidson, J. W. 1970. The energy balance of the global atmosphere. In: The global circu-lation of the atmosphere (ed. Corby, G. A), pp. 42–90. London: Roy. Met. Soc.
- Oort, A. H. 1964. On estimates of the atmospheric energy cycle. Mon. Wea. Re v. 92, 483–493.
- Peixoto, J. P. and Oort, A. H. 1992. Physics of climate. American Institute of Physics, 520 pp.
- Stull, R. B. 1988. An introduction to boundary layer meteorology. Kluwer Academic Publishers, 666 pp.
- Van Mieghem, J. 1956. The energy available in the atmosphere for conversion into kinetic energy. Beitr. Phys. Atmos. 29, 129–142.
- Van Mieghem, J. 1973. Atmospheric energetics. Oxford Monograph on Meteorology. Clarendon Press, 306 pp.
- Vinnichenko, N. K. 1970. The kinetic energy spectrum in the free atmosphere - one second to five years. Tellus 22, 128–166.
- Yamada, T. and Mellor, G. 1975. A simulation of the Wangara atmospheric boundary layer data. J. Atmos. Sc i. 32, 2309–2329.