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Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article

Classified by OpenAIRE into

arxiv: Physics::Atmospheric and Oceanic Physics, Physics::Space Physics
Correlation coefficients between the meridional wind and zonal wind and meridional wind and temperature measure the efficiencies of eddy transports of momentum and heat, respectively. Efficiencies are calculated in terms of these correlation coefficients for the major warming event of January 1977. It is found that the eddies are more efficient in transporting heat than in transporting momentum. Further, the efficiency of heat transport increased substantially before the meridional temperature gradient reversed. Increase of efficiency in heat transport is found to be related to the increased westward tilt of a wave in the height field. Since this tilt is known to be associated with vertical propagation of wave energy, interesting connections are inferred between the efficiencies of eddy transports, wave structure and energetics during a stratospheric warming.DOI: 10.1111/j.2153-3490.1981.tb01730.x
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    • Charney, J. G. and Drazin, P. G. 1961. Propagation of planetary scale disturbances from the lower into the upper atmosphere. J.Geophys. Res. 66,83-109.
    • Eliassen, A. and Palm, E. 1961. On the transfer of energy in stationary mountain waves. Geophys. Publ. 22 (3). 1-23.
    • Free University of Berlin. 1977. Daily northern hemisphere 50 and 30 mb synoptic weather maps of the year 1977. Freien Univ. Berlin.
    • Hartman, D. 1977. Comments on “stratospheric long waves: Comparison of thermal structure in the Northern and Southern Hemispheres”. J . A fmos. Sci. 3 4 , 4 3 4 4 3 5 .
    • Julian, P. R. and Labitzke, K. B. 1965. A study of atmospheric energetics during the January-February 1963 stratospheric warming. J. Atmos. Sci. 22, 597-6 10.
    • Matsuno, T. 1971. A dynamical model of the stratospheric sudden warming. J. Atmos. Sci. 2 8 , 1479- 1494.
    • Muench, H. S. 1965. On the dynamics of the winter time stratosphere circulation. J.Atmos. Sci. 2 2 , 262-283.
    • Murakami, T. 1965. Energy cycle of the stratospheric warming. in early 1958. J. Meteor. SOC.Japan 43, 262-283.
    • O'Neill, A. and Taylor, B. F. 1979. A study of the major stratosphere warming of 1976177. Quart. J. R . Met. SOC1.05,71-92.
    • Oort, A. H. and Rasmusson, E. M. 1971. Atmospheric circulation statistics, NOAA Prof. Pap. 5, 323 pp. (Available from Gov. Printing Office, stock No. 0 3 17-0045, C55.25.5.)
    • Quiroz, R. S. 1977. The tropospheric-stratospheric polar vortex breakdown of January 1977. Geophys. Res. Letters4, 151-154.
    • Reed, R. J. Wolfe, J. L. and Nagatani, R. M. 1963. A spectral analysis of the energetics of the stratospheric sudden warming of early 1957. J. Atmos. Sci. 20, 265-275.
    • Schoeberl, M. R. 1978. Stratospheric warmings: observations and theory. Rev. Geophys. and Sp. Phys. 16, 521-538.
    • Srivatsangam, S . 1975. On the efficiencies of atmospheric processes. Tellus 22, 365-370.
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