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EVAT 554 OCEAN-ATMOSPHERE DYNAMICS
LECTURE 5 EQUATION OF STATE; FILTERING OF EQUATIONS FOR ATMOSPHERE (Reference: Peixoto & Oort, Chapter 3)
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We still do not have a closed system of equations!
equation of state... Let us first consider the atmosphere…
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Recall Ideal Gas Law: For Dry Air: Define Thus, we can write:
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What about water vapor? Dalton’s Law of Partial Pressures:
For water vapor we can write: Where Take Thus, we can write:
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What about water vapor? Dalton’s Law of Partial Pressures:
For water vapor we can write: Where: Take Now define:
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What about water vapor? Take Now define:
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What about water vapor?
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What about water vapor? This equation of state has general validity for the atmosphere, for the current atmospheric composition
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Governing Equations for Atmosphere
Zonal Momentum Balance Meridional Momentum Balance Vertical Momentum Balance Continuity Equation of State Temperature Equation How many equations? How many variables?
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The Earth's Atmosphere from Space
The thin blue arc near the horizon shows the shallowness of the earth's atmosphere.
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Zonal Momentum Balance:
Length scale: L106m, l102m Depth scale: H104m, h 102m Horizontal velocity scale: u,v 10 ms-1 Vertical velocity scale: w 10-2 ms-1 Horizontal pressure scale: p 10 mb = 1000 Pa Time Scale: L/u 105s or H/w 106s Radius of Earth: a=6.37x 106m Coriolis parameter: f,f' 10-4 s-1 Density of Air: r 1 kg m-3 Horizontal Eddy Viscosity: nH 10-1 m2s-1 Vertical Eddy Viscosity: nV 10-1 m2s-1 10-4 ms-2 10-3 ms-2 10-6 ms-2 10-3 ms-2 10-4 ms-2 10-4 ms-2
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Meridional Momentum Balance:
Length scale: L106m, l102m Depth scale: H104m, h 102m Horizontal velocity scale: u,v 10 ms-1 Vertical velocity scale: w 10-2 ms-1 Horizontal pressure scale: p 10 mb = 1000 Pa Time Scale: L/u 105s or H/w 106s Radius of Earth: a=6.37x 106m Coriolis parameter: f,f' 10-4 s-1 Density of Air: r 1 kg m-3 Horizontal Eddy Viscosity: nH 10-1 m2s-1 Vertical Eddy Viscosity: nV 10-1 m2s-1 10-4 ms-2 10-3 ms-2 10-3 ms-2 10-4 ms-2 10-4 ms-2
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