with a prefontal thermodynamically PDF
12 Pages·2007·0.85 MB·English
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through a typical pre-existing, finite-amplitude disturbance prior to its amplification into an intense front-trough system. In brief, the initial state consists of a zonal shear flow in thermal wind balance (Eqns 1 and 2) in which is embedded a warm prefrontal northerly airstream, v(X,z;0) (for de
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