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Rao, Y. P. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
The mean meridional circulation is maintained by the eddy terms,. The magnitude of these terms in different latitudes is discussed.DOI: 10.1111/j.2153-3490.1967.tb01503.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

    • Brooks, C. E. P., Durst, C. S., Carruthers, N., Dewar, D. & Sawyer, J . S. 1950. Upper winds over the world. Geophysical Memoirs, London, Vol. 10, N o . 85.
    • CROSSLEAY.,F. 19.50.Relation between the standard deviations of temperature at constant pressure and at constant height. Quarterly Journal Royal Met. SOC.7 6 , 337-340.
    • Goldie, N., Moore, J. G. & Austin, E. E. 1958. Upper air temperature over the world. Geophysical M e - moirs, London, 13, N o . 101.
    • Heastie, M. & Stephenson, P. M. 1960. Upper winds over the world. Geophysical Memoirs, London, 13, No. 103.
    • Palmen, E. & Vuorela, L. A. 1963. On the mean meridional circulations in the Northern Hernisphere during the winter season. Quarterly Journal Royal M e t . Soc. 89, 131-138.
    • Rao, M. S. V. 1963. Mean meridional air-motion and associated transport processes in the atmosphere. I n d i u n Journal of Met. and Geophysics 14, 117- 142.
    • Starr, V. P. & White, R. M. 1954. Balance requirements of the general cirrulation. Geophysics Res. papers, No. 35. Cambridge,U.S.A.
    • Tucker, G. B. 1959. Mean meridional circulations in the atmosphere. Quarterly Journal of Royal Met. SOC.8;, 209-224.
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