Atmospheric and Oceanic Sciences Program Princeton University
Course: AOS 572 Atmospheric and Oceanic Waves Spring 2005.
1.) Introduction to Mountain Effects, Scale -analysis.
a.1 Quasi Geostrophic response
a.2 QG equations, Potential Vorticity
a.3 Steady solutions for a bounded fluid and semi-infinite
Atmosphere.
b.1 Barotropic Response, Rossby waves.
b.2 The response on a channel flow in a beta-plane.
b.3 Numerical simulations.
IIa. Regional and Planetary Scales.
a.1 Barotropic Instability, necessary condition for instability,
interacting two edge waves.
a.2 Baroclinic Instability, Uniform PV The Eady Model.
a.3 Instability on a beta-plane, the Charney Model.
a.4 The life-cycle of a normal mode. Eddy energy cycle
b.1 Eddies in zonally asymmetric flows. Downstream development,
Energy fluxes and group velocity.
b.2 Fronts and Frontogenesis
b.3 Wave-breaking, anticycloninc and cyclonic breaking, effect into
the larger-scale flow (feedback into the quasi
stationary circulation).
b.4 life-cycle of baroclinic eddies in the Storm Tracks.
b.5 Meanders of ocean currents, mesoscale eddies.