Geophysical Fluid
Dynamics-1 Winter 2001 OC 512a/ ATM 509 SLN: 5814
lectures: MWF 9.30-10.20; OSB room 425
lab demo hour: F 10.30; OTB room 206 or OSB
107
P.B. Rhines rhines@ocean.washington.edu Ocean Sciences room 319 tel 3-0593
L. Thomas leif@ocean.washington.edu Ocean Sciences room 308 tel 3-0769
Web site: www.ocean.washington.edu/courses/oc512
OUTLINE (associated math in bold text)
==========================
oceans and atmospheres: general description
buoyancy, pressure, stable stratification, mean vertical structure
rotation, geopotential, Coriolis force
scale analysis
geostrophic balance
equations of motion;
Cartesian
sphere
adiabatic; diabatic => basic thermodynamics
particle on an f-plane
long gravity waves with rotation method of
characteristics
waves; Poincare, Kelvin
waves and circulations
hydrostatic
balance forced/free solutions (homogeneous/particular)
geostrophic adjustment-I
geostrophic flow
Rossby deformation radius
energetics
rotational stiffness
Ekman layers – I boundary-layer (singular
perturbation) theory
wind-driven channel flow
meridional circulation
continuously stratified fluids
geostrophic adjustment-II
thermal wind
Prandtl ratio, Burger number
potential/kinetic energy
velocity spirals
internal waves
Boussinesq, atmos model with compressibility
group velocity ‘wave mathematics’: multi-scale
analysis (‘two-timing’); Fourier analysis; eigenmodes, eigenvalues
mountain waves
modes and turning points with non-uniform stratification
vorticity and potential vorticity (pv-) dyamics
Kelvin’s and Bjerknes circulation theorems
em analogies
spin and angular mom
vorticity and pv inversions
vortex stretching and tipping
Ekman layers – II: spin-up
Rossby waves I: single-layer fluid
pv robustness, Ń·J; conservation, sources and sinks
energy dissipation; enstrophy dissipation
transport of scalar and vector quantities by waves and eddies
geostrophic scaling: regular pert theory => perturbed
eigenvalue
synoptic QG (quasi-geostrophic) equation:
QG flow over a mountain
potential vorticity production: Shaer, lab..
thermally forced vortex; convection -I
Rossby waves-II
Some extra topics, if time permits:
baroclinic energy conversion
meridional circulations
convection –II: convective heat transport
in boundary layers
at global scale chaos:
low-order, nl systems
intense eddies, vortices
vortex pair
merger, 2DT
vortex stretching limited
thermally forced vortex
hydraulics
downslope flow, solitons, undular bore
advection/diffusion
similarity variables
==========================
LABS (not
necessarily in this order)
1. Pressure, buoyancy, eqn of state, heat content and flux; surface effects, evaporation, droplets; low-pressure fluids: boiling and freezing, clinking, latent heat transport in 2-chamber vessel.
2. Waves-I Overhead projector ripples, mean flow. U-tube; one- and two-layer gravity waves, particle paths; wave packet, group velocity; solitons, gravity current, mean flows; piano and surface tension modes
3. Coriolis effects: equilibrium geoid; stiff columns; Taylor Proudman, Coriolis force on a jet; inertial waves; Kelvin waves/gravity current; tornado vortex, rotating flow over mountain
4. Geostrophic flow, geostrophic adjustment in a channel (Gill), geostrophic adjustment of cylindrical blob; thermal wind shear (narrow gap annulus exp); river outflow plume.
5. Ekman layers and spin-up. Boundary layers, Ekman veering; Wedding cake (vertical shear layers); sink flow (purple tornado); spin-up time (energetic argument); effects of stratification; coastal upwelling, fronts
6. Waves –II continuous stratification, int. grav waves, mountain waves
hydraulics, estuary model, kitchen sink bore, 8’ flume undular bores, numerical model
7. Stirring and mixing and their dynamical products. Basic diffusion of heat and dye in a column; heat and tracer flux enhanced by fluid strain (onion slice with fluorescein); stirring and mixing; convection and boundary layers; turbulent jet entrainment; estuary; double diffusion and layering.
8. Global heat engine, meridional circulation, heat flux and baroclinic instability. rotating annulus exper: narrow (stable zonal flow)/med (wave regime; jets and eddies) /wide gap (geost. turbulence) Thermal wind measured; non-rotating slot
9. Rossby waves and potential vorticity. Polar b plane; induced zonal jets, polar vortex; oscillatory Charney-deVore (Boris ridge-ed bowl); barotropic instability, vortex interactions.
TEXT:
Gill, A.E., Atmosphere-Ocean Dynamics, Academic Press
OTHER REFERENCES
Pedlosky, J., Geophysical
Fluid Dynamics, Springer
Verlag (complements Gill, emphasizing
QG dynamics, Rossby waves, baroclinic instability, non-dimensional scaling)
Acheson, D. Elementary Fluid Mechanics, Oxford Univ. Press (excellent, terse
introduction to classical fluid mechanics)
Lighthill, M.J., An informal introduction to theoretical
fluid mechanics. Oxford Univ. Press (especially expert
discussion by a master of vorticity,
and of sound propagation)
Lighthill, M.J., Waves in Fluids. Cambridge Univ. Press (basic
wave mathematics, of non-dispersive and
dispersive wave types; ray-tracing; internal and Rossby waves).
Whitham, G.B. Linear and Nonlinear Waves. Wiley and Sons (a remarkable presentation of
non-dispersive and dispersive waves from a fundamental mathematical point of
view).
Salmon, R., Lectures on
Geophysical Fluid Dynamics, Oxford
Univ. Press (another remarkable, recent text treating mostly large-scale QG
oceanic GFD but with
fundamental ideas
about fluid dynamics based on Hamilton’s principle)
James, I., Introduction to
Circulating Atmospheres (readable
discussion of basic GFD of the large-scale atmosphere)
Batchelor,G.K., An Introduction to Fluid Dynamics, Cambridge
Univ. Press (impeccable reference on basic incompressible fluids, vorticity,
strain, boundary layers)
Kundu,P. Fluid Dynamics, Academic Press (includes sections on elementary GFD)
Tritton, D., Physical Fluid Dynamics (basic fluids from a GFD point of view).
Van Dyke,M. An Album of
Fluid Motion, Parabolic Press (amazing photographs of basic fluid
dynamics).
Landau and Lifshitz, Fluid Mechanics, Addison-Wesley (an early treatment of fluid dynamics by two great physicists).