CLIM 711 Introduction to Dynamic Meteorology
Instructor: E. K.
Schneider
Text
- Holton, J. R., An Introduction to Dynamic Meteorology, 3rd or 4th
edition.
Prerequisites
- Newtonian physics, vector calculus, partial
differential equations
Course work:
- Lectures
- Reading of appropriate sections in text
- Weekly problem sets
- Midterm and final exams
1. Laws of motion (Chap. 1)
- Fundamental forces
- Gravitational, pressure gradient, friction, Coriolis
- Mixing length theory, molecular vs. eddy
viscosity
- Structure of the static atmosphere
- Generalized vertical coordinate, pressure
vertical coordinate
2. Basic conservation laws (Chap. 2)
- Total differentiation, Eulerian
and Lagrangian reference frames
- Total derivative of vector
- Rotating frame
- Conservation of momentum in spherical coordinates
- Conservation of mass
- Conservation of energy
- Potential temperature, adiabatic lapse rate
- Static stability
- Scale analysis
- Hydrostatic balance
- Geostrophic balance
- Primitive equations in z coordinates
- Primitive equations in pressure coordinates
- Geostrophic balance
- Thermal wind
- Barotropic flow
3. Circulation and vorticity (Chap. 4)
- Bjerknes theorem (general case)
- Kelvin theorem (barotropic
case)
- Relative circulation
- Conservation of angular momentum and ideal
Hadley circulation (*)
- Absolute vorticity,
relative vorticity
- Natural coordinates: shear and curvature
- Local Cartesian coordinates
- Conservation of potential vorticity
- Examples
- Barotropic (conservation of absolute vorticity)
- Baroclinic mountain forced
- Absolute vorticity eqn.
- Relative vorticity eqn. (vertical component)
- Scale analysis
- Ertel potential vorticity
- Barotropic vorticity eqn.
- Fourier analysis (Sec. 7.2.1)
- Free Rossby waves in
1D and 2D (Sec. 7.7.1)
- Topographically forced Rossby
waves (Sec. 4.5, 7.7.2)
4. Boundary layer and turbulence (Chap. 5)
- Reynolds averaging
- Boussinesq equations
- Bulk formulae
- Vertically integrated boundary layer
- Ekman layer
o Ekman pumping
o Secondary circulations and spin down
o Parameterization of surface boundary layer in barotropic vorticity equation
o Topographically forced Rossby
waves with friction
·
Group velocity
and dispersion (Sec 7.2.2)
5. Quasi-geostrophic
theory
- Derivation of quasi-geostrophic
potential vorticity equation (Sec 6.2)
- 2-layer model of barclinic
instability (Sec. 8.2)
- Equations of motion in log-pressure coordinates
(Sec. 8.4.1)
- Extratropical energy cycle (Sec. 10.4)
- Rossby waves in 3 dimensions (Sec. 10.5.1)
6. Waves (Chap. 7)
- Acoustic waves
- Shallow-water gravity waves
- Internal gravity waves
- Inertio-gravity waves
- Adjustment to geostrophic
balance
Last modified 15 December 2005