Atmospheric Circulation Systems: Their Structure and by E. Palmén and C.W. Newton (Eds.)

By E. Palmén and C.W. Newton (Eds.)

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Quart. J. Roy. Meteorol. Soc. 52, 85-104. -K. (1954). The meridional transport of kinetic energy in the atmosphere. J. Meteorol. 11, 352-361. Krishnamurti, T. N. (1961). The subtropical jet stream of winter. J. Meteorol. 18, 172-191. Kuo, H. L. (1951). A note on the kinetic energy balance of the zonal wind systems. Tellus 3, 205-207. Lorenz, E. N. (1967). " World Meteorological Organization, Geneva. Machta, L. (1949). Dynamic characteristics of a tilted-trough model. J. Meteorol. 6, 261-265. Mintz, Y.

Meteorol. 11, 352-361. Krishnamurti, T. N. (1961). The subtropical jet stream of winter. J. Meteorol. 18, 172-191. Kuo, H. L. (1951). A note on the kinetic energy balance of the zonal wind systems. Tellus 3, 205-207. Lorenz, E. N. (1967). " World Meteorological Organization, Geneva. Machta, L. (1949). Dynamic characteristics of a tilted-trough model. J. Meteorol. 6, 261-265. Mintz, Y. (1951). The geostrophic poleward flux of angular momentum in the month January 1949. Tellus 3, 195-200. Mintz, Y.

This takes account of the convergence of meridians. 6) We can also include the latent heat in the atmospheric energy flux. By release upon condensation of the vapor, this energy form goes over into internal and potential energy. 7) where q is specific humidity. The formula is strictly valid if no change in storage of water vapor occurs and all water vapor condensed immediately precipitates. If the latent heat is included in the atmospheric energy flux, Eq. 8) + where W~a represents the atmospheric flux of (cpT + (/J Lq), which C.

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