What is baroclinicity in climatology?


What is baroclinicity in climatology?


Baroclinicity is a concept in fluid dynamics that measures how misaligned the gradient of pressure is from the gradient of density in a stratified fluid. This causes instability in the fluid with a resultant greater tendency for motion to correct it.

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The atmosphere is a specific case of fluid dynamics since it behaves like a large-scale fluid. Baroclinicity in the atmosphere is when atmospheric...

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Atmospheric Circulation: Scale & Observation


Chapter 9 / Lesson 1

Atmospheric circulation is caused by different flows of air due to heat regions in the earth's atmosphere. Learn more about atmospheric circulation and explore the different scales and observations related to atmospheric circulation.

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