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Jet Stream
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Wasaburo Oishi, Japanese Discoverer (1920s)
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Fu-Go Balloon Weapon
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Strahlstromung (German) for “jet stream” first used in 1939
Big effects on bomber flights during WWII
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Jet Stream winds are not uniform
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250 mb isotach
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Main Upper Tropospheric Jets Closely Associated with the Tropopause
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Tropopause
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Tropopause Height http://www.atmos.washington.edu/~hakim/tropo/tropo.html
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Subtropical Jet Stream
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Subtropical Jet Stream Often Associated with a cloud band
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http://itg1. meteor. wisc
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Jet Stream’s Relationship to Temperature Can Be Shown through Thermal Wind Arguments
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250 mb isotach
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1000-500 mb thickness-large thickness gradient and thus thermal wind near jet core
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Or alternatively…
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The Jet Stream Recall the horizontal temperature effects
on the pressure: 500 mb 700 mb 850 mb Psurface Warm Cold
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The Jet Stream Consider the balance of forces at each level: Co PGF
500 mb 700 mb 850 mb Ps Warm Cold
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There are a variety of jet stream configurations that are well-known
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