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In Fic. 6, shown above is a cross-section by Van Mieghem based on 
a series of consecutive soundings at Uccle, Belgium, and a few nearby sta- 
tions, shows a very shallow cold air tongue and an open warm sector, with 
the accompanying clouds, surface and stratosphere weather changes. The typical 
multiple tropopauses and stratosphere changes are present but not nearly so 
pronounced as over a deep cyclone. The surface weather follows a very ideal 
course according to the original Bjerknes scheme of 1919. [Dotted lines are 
inversions of subsidence (in the troposphere) and diffuse tropopauses (at high 
levels) ; temp. in degrees Abs.; clouds stippled.] (From: Mem. Inst. Roy. Met. 
Belg., v. 12, 1939.) 
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