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Berkofsky, Louis (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
It is shown that, if the equations for an n-level model are averaged, the resulting equations have mathematical forms which, under certain conditions, are identical with those of the vertically integrated n-parameter model. The implications for the temperature and ω-profiles are discussed in order to achieve exact mathematical equivalence. A physically consistent vertically integrated model yields temperature and ω-profiles which depart from those required for mathematical exactness, yet appears to lead to more realistic results.DOI: 10.1111/j.2153-3490.1963.tb01405.x
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    • BERKOFSKLY., 1958, A three-parameterbaroclinic numerical prediction model, Journ. Met., 18, pp. 102-1 11.
    • CHARNEY,J., and PHILLIPSN,., 1953, Numerical integration of the qua&-geostrophic equations for barotropic and simple baroclinic flows, Journ. Met., 10, pp. 71-99.
    • ELLIASSENA,., and KLEINSCHMIDET.,,1957. Dynamic meteorology, in Handbuch der Phyaik, Band XLVIII, Geophysik 11, pp. 1-154.
    • KNIGHTINGE,., 1980, Some computations of the variation of vertical velocity with pressure on a synoptic scale, QJRMS, 86, pp. 318-328.
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