Abstract
The characteristics of the observed seasonal mean flow of the atmosphere for December–February and June–August are discussed. Various models and sets of equations are used to investigate the importance of orographic and thermal forcing and the role played by transients on the synoptic and longer time-scales.
The usefulness of considering maps of potential vorticity on isentropic surfaces for the diagnosis of the behaviour of synoptic systems in the atmosphere is illustrated.
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© 1986 D. Reidel Publishing Company, Dordrecht, Holland
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Hoskins, B.J. (1986). Some Topics in the General Circulation of the Atmosphere. In: Willebrand, J., Anderson, D.L.T. (eds) Large-Scale Transport Processes in Oceans and Atmosphere. NATO ASI Series, vol 190. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-4768-9_2
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DOI: https://doi.org/10.1007/978-94-009-4768-9_2
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