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ATOC 4720 class 39 Thermally driven circulation with the influence of planetary rotation.

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Presentation on theme: "ATOC 4720 class 39 Thermally driven circulation with the influence of planetary rotation."— Presentation transcript:

1 ATOC 4720 class 39 Thermally driven circulation with the influence of planetary rotation

2 Previous class: without rotation (f=0)
LAB EXP: Net+Latent heat EQ North Pole

3 Atmosphere: Symmetric Hadley Cells (f=0)
High P Pressure High P High P Low P

4 OBSERVATIONS: WINTER EQ

5 SUMMER

6 Angular momentum, equation, and conservation
Air parcel: unit mass

7 Conservation: ideal case: P is independent of longitude: No friction
Equation: Friction Conservation: ideal case: P is independent of longitude: No friction =constant

8 Assume an air parcel at EQ, u=0
Westerly winds! Geostrophic winds: parallel to isobars!

9 Maintenance of geostrophic balance: Frictionless
Quasi-geostrophic motion Convergence Divergence Z-coordinate: If

10 Maintenance of thermal wind equilibrium

11 In the previous class: Primitive equations:
( )


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