週次 |
日期 |
單元主題 |
第1週 |
|
Course introduction, paper assignment |
第3週 |
3/16 |
Review of Quasi-Geostrophic PV conservation and Rossby waves
1. QG (single layer)
a. fdshort.pdf page 61-73
b. John Taylor's note Ch. 3
2. QG (stratified)
a. fdshort.pdf page 85
3. Rossby waves
a. fdshort.pdf Ch. 4.1-4.3
b. Taylor's note Ch. 4.0
|
第5週 |
3/30 |
Motivations: observations of surface westerlies ---- Fucent Hsu
To read (in 311840_Vallis_3.pdf)
1. The Ferrel Cell (Ch. 14.7)
2. Surface westerlies (Ch. 15.1)
Other ref:
Issac Held's WHOI lecture (section 1) |
第7週 |
4/13 |
Eddy vorticity and momentum fluxes in linearized equations (Ch. 10.1, 10.2, 10.3) |
第9週 |
4/27 |
mid-term week |
第10週 |
5/4 |
Dr. Pei-Chun Hsu's talk on zonal flow formation & PV fluxes |
第11週 |
5/11 |
Eliassen-Palm flux (Ch. 10.2)
Mean-flow momentum equation: The Transformed Eulerian Mean (TEM) (Ch. 10.3) |
第12週 |
5/18 |
Eliassen-Palm flux (Ch. 10.2)
Mean-flow momentum equation: The Transformed Eulerian Mean (TEM) (Ch. 10.3)
E-P fluxes (Hoskins book chapter 16) --- by 林悅琪 林沅箴 |
第14週 |
6/1 |
Review sets of equations for wave-mean-flow interactions
1. QG momentum --- Rossby-number expansion, filtering out inertial gravity waves
2. QGPV
3. mean PV conservation ( dq_bar/dt = -d/dy(v'q'); d = partial derivatives)
4. linearized q' evolution eq
(dq'/dt + ubar dq'/dx + v' dq_bar/dy = 0)
5. v'q' = divergence of E-P flux
6. Wave activity conservation
dA/dt + v'q' = 0
v'q' = div of F
7. Transformed Eulerian Mean --- Lagrangian averaging in the vertical
8. Interpretation for E-P flux
(1) F = Cg*A --- as wave energy flux
(2) du/dt -fva = div of F (TEM mom) --- as easterly momentum flux |
第16週 |
6/15 |
1. Interpretation for E-P flux (continued)
2. Eddy form stress: what does it mean ?? (Ch. 10.4)
3. Ceppi et al. (2013) |
第17週 |
|
Synthesis
Application to the Eady problem (Ch. 10.5) |