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Srivatsangam, S. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
Harmonic analysis of the standing-eddy transport of sensible heat in the Northern Hemisphere polar latitudes shows that the equatorward sensible heat transfer in these latitudes in January is due to different zonal harmonics at different latitudes and isobaric levels. A comparison of the transports of sensible heat by the standing eddies, up the meridional temperature gradient, in the midlatitude lower stratosphere and the polar troposphere, shows that these up-gradient transports are due to different mechanisms. The former is caused by a relative maximum of time-and-zonal average temperature in the midlatitude stratosphere which owes itself to the mean meridional circulation, and does not involve any meridional changes in the structure of the standing eddies; but the latter is due to cross-latitude changes in the direction of tilt of the vertical axis of the standing eddies.DOI: 10.1111/j.2153-3490.1975.tb01665.x
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    • Lorenz, E. N. 1951. Computetions of the balance of angular momentum and the poleward transport of heat. Sci. Rep. No. 6, M.I.T. General Circulation Project, 34 pp.
    • Miyakoda, K. 1963. Some characteristic features of winter circulation in the troposphere and lower stratosphere. Department of Geophysical Science, University of Chicago, Tech. Rep. No. 14, 93 pp.
    • Oort, A. H. & Rasmusson, E. M. 1971. Atmospheric circulation statistics, Rockville, Md., U.S. Department of Commerce, 323 pp.
    • Reed, R. J., Wolfe, J. L. & Nishimoto, H. 1963. A spectral anslysis of the energetics of the stratospheric sudden warming of early 1957. J. Atmos. Sc. 20, 256-275.
    • Van Mieghem, J. 1961. Zonal harmonic analysis of the Northern Hemisphere geostrophic wind field. International Union of Geodesy and Geophysics, Monographie No. 8, 57 pp.
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