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Holmboe, Jörgen (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:

Classified by OpenAIRE into

arxiv: Physics::Atmospheric and Oceanic Physics
In a two-layer model of the atmosphere with the upper warm air moving from the west relative to the cold air below the long waves are unstable and have a rather simple symmetric structure and behavior when the following approximations are used: (a) The latitude variation of the depth of the layers is ignored. (b) The motion is quasigeostrophic. (c) The planetary ?-gradient of the earth's vorticity is ignored. (d) The tropopause is a rigid horizontal surface. When these approximations are removed one by one the wave structure and growth rate are modified somewhat, but the essential features of the wave mechanism remain unchanged.DOI: 10.1111/j.2153-3490.1966.tb00304.x
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    • EADY,E. T., 1949, Long waves and cyclone waves. Tellwr, 1.No. 3.
    • BJERKNESJ,., 1937, Theorie der aussertropischen Zyklonenbildung. Met. Z e d , 12.
    • ROSSBY,C. G., and collaborators, 1939, Relation between the intensity of the zonal circulation of the atmosphere and the displacements of the semipermanent centers of action. J . Mar. Res. 2, No. 1.
    • LORDRAYLEIOHS,cientific Papers, 9, p. 575.
    • POCT 3APOXAAIOIIJEnCFI m P O H T A J I b H O n BOJIHbI
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