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Barotropic instability - PowerPoint PPT Presentation

Measuring and Predicting Practical 2: atmospheric dynamics

Measuring and Predicting Practical 2: atmospheric dynamics. Dr Paul Connolly Centre for Atmospheric Science. Motivation: last week we said that turbulence / fluid motions mix pollutants in the atmosphere. This week we will learn about what causes some of these fluid motions. Topics covered.

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Baroclinic Instability

Baroclinic Instability. Trough. Ridge. Southerlies. Northerlies. H. L. Cold. Warm. H. L. Baroclinic Instability. Baroclinic Instability Basic Idea Simple Models Classic Eady Framework Contributions from Barotropic Instability Examples of Observational Evidence.

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1.92k views • 20 slides

b 0 =0

Sverdrup interior. ? 2 p + [(2*H* b 0 )/(d *|f 0 |)] ? x p + [2/d ] f 0 /|f 0 | ? y t (x) = 0. Stommel boundary. Vorticity:. b 0 =0. b 0 >0. -p ( x,y ). t (x). f -plane:. b -plane:. f const x const. f + x -. f const x const. f - x +. f + x = const. f + x = const.

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250 views • 7 slides

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Barotropic instability - PowerPoint PPT Presentation

Measuring and Predicting Practical 2: atmospheric dynamics

Baroclinic Instability

b 0 =0