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Because this deflection of flow prevents a rapid filling of cyclones and a rapid
destruction of anti - cyclones , such pressure systems may remain active for many
days as will the jet streams with which they are associated ( Figure 3 ) .
Velocity and vorticity of flow argued that the jet streams generate their own frontal
zones , and not vice versa . Polar - Front and ... Well - defined wind - speed
maxima and minima are superimposed upon the jet stream belts . Thus , the air ...
The Tropical Easterly Jet Stream is closely connected with the Indian and African
summer monsoon . During winter the polar stratosphere cools appreciably
because of the lack of solar radiation . The ensuing strong horizontal temperature
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This is the 198215th Edition, in two halves, with the Macropaedia and the Micropaedia. First published in 1768, the publisher is the oldest English-language encyclopedia still in print. Two Scottish ... Read full review