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Published byHorace Jacobs Modified over 6 years ago
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ATOC 4720 class 39 Thermally driven circulation with the influence of planetary rotation
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Previous class: without rotation (f=0)
LAB EXP: Net+Latent heat EQ North Pole
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Atmosphere: Symmetric Hadley Cells (f=0)
High P Pressure High P High P Low P
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OBSERVATIONS: WINTER EQ
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SUMMER
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Angular momentum, equation, and conservation
Air parcel: unit mass
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Conservation: ideal case: P is independent of longitude: No friction
Equation: Friction Conservation: ideal case: P is independent of longitude: No friction =constant
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Assume an air parcel at EQ, u=0
Westerly winds! Geostrophic winds: parallel to isobars!
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Maintenance of geostrophic balance: Frictionless
Quasi-geostrophic motion Convergence Divergence Z-coordinate: If
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Maintenance of thermal wind equilibrium
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In the previous class: Primitive equations:
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