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Palmén, E.; Alaka, M. A. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article

Classified by OpenAIRE into

arxiv: Physics::Atmospheric and Oceanic Physics
A complete budget of angular momentum in the atmosphere is possible only by considering both the eddy transfer of angular momentum and the transport due to “mean meridional circulations”. An attempt has been made in the present paper to achieve such a complete budget for the zone 20–30°N using the data available. The mean mass transport in the tropical circulation cell accumulates high relative momentum (W wind) in the upper atmosphere of this belt, whereas the eddy transport distributes it northwards and downwards from this subtropical jet.DOI: 10.1111/j.2153-3490.1952.tb01020.x
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    • JORDANC,. L., 1952: A Comparison Between Observed and Geostrophic Winds in Low Latitudes. (To be published.)
    • MINTZ,Y., 1951: The Geostrophic Poleward Flux of Angular Momentum in the Month of January, 1949. Tellus, 3. pp. 195-200.
    • PALM~EN., 1951:The Role of Atmospheric Disturbances in the General Circulation. Quarf. /. Roy. Met. SOC., 77, pp. 337-354.
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    • RIEHL,H., and YEH,T. C., 1950: The Intensity of the Net Meridional Circulation. Quart. J. Roy. Met. SOC., 76, pp. 182-188.
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    • STARRV,. P., 1948: An Essay on the General Circulation of the Earth's Atmosphere. /. ofMet., 5. pp. 3-43.
    • STARRV,. P., and WHITE, R. M., 1952: Meridional Flux of Angular Momentum in the Tropics. Tellus, 4, pp. 118-125.
    • WIDCERW,. K., 1949: A Study of the Flow of Angular Momentum in the Atmosphere. 1. of Mef., 5, pp 291-299.
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