The New Encyclopędia BritannicaEncyclopędia Britannica, 1983 - Encyclopedias and dictionaries |
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Page 162
... stream band that surrounds the polar cylinder symmetrically . Because of frictional forces acting in the vicinity of the polar cylinder , the jet stream will not touch the ... jet streams generate their own frontal zones 162 Jet Streams.
... stream band that surrounds the polar cylinder symmetrically . Because of frictional forces acting in the vicinity of the polar cylinder , the jet stream will not touch the ... jet streams generate their own frontal zones 162 Jet Streams.
Page 163
... jet streams generate their own frontal zones , and not vice versa . Polar - Front and Subtropical Jet Streams do not sur- round the hemispheres in bands of uniform wind speeds . Well - defined wind - speed maxima and minima are super ...
... jet streams generate their own frontal zones , and not vice versa . Polar - Front and Subtropical Jet Streams do not sur- round the hemispheres in bands of uniform wind speeds . Well - defined wind - speed maxima and minima are super ...
Page 164
... 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 gradient in the ...
... 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 gradient in the ...
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