Atmospheric and Oceanic Sciences 576
Topics in Dynamical Meteorology
The General Circulation of the Atmosphere
Dr. Isaac M. Held
Senior Research Scientist
Geophysical Fluid Dynamics Laboratory
National Oceanic and Atmospheric Administration
P. O. Box 308, Princeton, NJ 08542 USA
Lecturer
Program in Atmospheric and Oceanic Sciences
Department of Geosciences
Princeton University
Lectures 8:30 - 10:00, Monday and Wednesday , Room 219, Guyot Hall
Click on the following to see lecture notes from a summer school; these give a good indication of the kinds of problems that will be addressed in the course.
Lecture Notes on the General Circulation of the Atmosphere: Woods Hole GFD Summer School, 2000
See also
Tokyo lectures 2002
Course Outline
Background reading
Dennis Hartmann review
Tapio Schneider review
Lorenz -- Nature and Theory of the General Circulation of the Atmosphere
Schneider and Sobel -- The Global Circulation of the Atmosphere
Vallis -- Atmospheric and Oceanic Fluid Dynamics, particularly Chapters 11-13.
Goals:
develop intuition for how the climate of the atmosphere is controlled
isolate interesting unsolved problems
Topics (tentative- to be revised soon):
Review of circulation, vorticity, potential vorticity
2D non-divergent flow on the sphere
Vorticity mixing, zonal mean acceleration, pseudomomentum, and the Earth's angular momentum balance
Rossby waves
meridional propagation, WKB
pseudo-momentum, pseudo-energy, orthogonality of normal modes
instability, over-reflection
critical layers
ray tracing -- relation to observed teleconnection patterns
edge waves, pseudo_energy conservation, and storm tracks
Shallow water equations
quasi-geostrophy
orographic forcing, mountain torque, and the non-acceleration theorem
The quasi-geostrophic two-layer model
Intro to baroclinic instability, Charney-Stern, pseudomomentum
"PV thinking"
"Transformed Eulerian" momentum budget
qualitative picture of the mainenance of the global circulation
The Hadley cell and the subtropical jet
linear and nonlinear axisymmetric models
the gross moist stability
the intertropical convergence zone
atmospheric vs oceanic energy transport
Rossby wave- Hadley cell interaction
quasi-geostrophic wave-mean flow interaction theory
form drag and the Elliasen-Palm flux
the surface branch of the overturning mass-circulation
potential vorticity mixing and the general circulation
maintenance of tropospheric static stability and the tropopause
radiative and dynamical constraints
Tropics
Midlatitudes
Vertically propagating planetary waves and stationary eddies
beta-plane propagation and trapping
the external mode
orographic vs. thermal forcing in midlatitudes
the extratropical response to El Nino
Linear and finite amplitude baroclinic instability
2-layer, Eady, Charney
PV thinking
Baroclinic adjustment, amplitude bounds
the "barotropic governor"
the homogeneous limit
Geostrophic turbulence and scale selection
jet creation
Gravity waves and the QBO (if time permits)
gravity-wave mean flow interaction
Plumb's non-rotating QBO
equatorial waves
Isaac M. Held (Isaac.Held@noaa.gov) 609-452-6512