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

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

Jet Stream

250 mb isotach

Main Upper Tropospheric Jets Closely Associated with the

Tropopause

Tropopause

Tropopause Height

http://www.atmos.washington.edu/~hakim/tropo/tropo.html

Subtropical Jet Stream

Subtropical Jet Stream Often Associated with a cloud band

• http://itg1.meteor.wisc.edu/wxwise/AckermanKnox/chap7/subtropical_jet.html

Jet Stream’s Relationship to Temperature Can Be Shown

through Thermal Wind Arguments

250 mb isotach

1000-500 mb thickness-large thickness gradient and thus thermal wind near jet core

Or alternatively…

The Jet Stream

Recall the horizontal temperature effectson the pressure:

500 mb

700 mb

850 mb

Warm Cold Psurface

The Jet StreamConsider the balance of forces at each level:

500 mb

700 mb

850 mb

Warm ColdPs

PGFCo

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

known