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

By E. Palmén and C.W. Newton (Eds.)

ISBN-10: 0125445504

ISBN-13: 9780125445504

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Meteorol. Soc. 78, 583-589. Smagorinsky, J. (1963). General circulation experiments with the primitive equations: I. The basic experiment. Monthly Weather Rev. 91, 99-164. Starr, V. P. (1948). An essay on the general circulation of the earth's atmosphere. J. Meteorol. 5, 39-48. Starr, V. P. (1953). Note concerning the nature of the large-scale eddies in the atmosphere. Tel/us 5, 494-498. Starr, V. , and White, R. M. (1951). A hemispherical study of the atmospheric angularmomentum balance. Quart.

Quart. J. Roy. Meteorol. Soc. 75, 28-40. Priestley, C. H. B. (1951). A survey of the stress between the ocean and the atmosphere. Australian J. Sci. Res. A4, 315-328. Reed, R. , and Mercer, J. M. (1962). Arctic forecast guide. NWRF 16·0462·058, 107 pp. U. S. Naval Weather Research Facility, Norfolk, Virginia. Reynolds, O. (1894). On the dynamical theory of incompressible viscous fluids and the determination of the criterion. Phil. Trans. Roy. Soc. London A196, 123-164. , and Yeh, T. C. (1950). The intensity of the net meridional circulation.

It should be noted that Eq. 3) gives the flux at a particular instant. 3') Here the tilde indicates a mean over a period of time. ) term expresses the influence of the mean meridional circulation averaged over a period of time, and the second term (where the asterisks indicate a deviation of the longitudinally averaged u and v from the longerterm means) represents the contribution of the time variation of the mean meridional circulation. ; following discussion that iiv = {Hf and u'v' = u'v' . Several attempts have been made to compute the eddy flux of momentum, using principles formulated by Priestley (1949) and others.

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

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