Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause.

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Jet Stream

Transcript of Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause.

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Jet Stream

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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.edu/wxwise/AckermanKnox/chap7/subtropical_jet.html

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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 effectson the pressure:

500 mb

700 mb

850 mb

Warm Cold Psurface

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The Jet StreamConsider the balance of forces at each level:

500 mb

700 mb

850 mb

Warm ColdPs

PGFCo

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There are a variety of jet stream configurations that are well-

known

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