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Jet Stream

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

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Page 1: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

Jet Stream

Page 2: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

250 mb isotach

Page 3: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause
Page 4: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

Main Upper Tropospheric Jets Closely Associated with the

Tropopause

Page 5: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

Tropopause

Page 6: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

Tropopause Height

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

Page 7: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause
Page 8: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

Subtropical Jet Stream

Page 9: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause
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Subtropical Jet Stream Often Associated with a cloud band

Page 12: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

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

Page 13: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause
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Page 16: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

Jet Stream’s Relationship to Temperature Can Be Shown

through Thermal Wind Arguments

Page 17: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

250 mb isotach

Page 18: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

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

Page 19: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

Or alternatively…

Page 20: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

The Jet Stream

Recall the horizontal temperature effectson the pressure:

500 mb

700 mb

850 mb

Warm Cold Psurface

Page 21: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

The Jet StreamConsider the balance of forces at each level:

500 mb

700 mb

850 mb

Warm ColdPs

PGFCo

Page 22: Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause

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

known

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