- Chapter 3 Variable Basic States - 3.1 WKBJ analysis (1)
- 3.1 WKBJ analysis (2)
- 3.1 WKBJ analysis (3)
- 3.1 WKBJ analysis (4)
- 3.2 Critical level behavior
- 3.2.1 Richardson number
- 3.2.2 Conditions for absorption
- 3.2.3 Linear and nonlinear limits (1)
- 3.2.3 Linear and nonlinear limits (2)
- 3.3 Damping and momentum deposition
- 3.3.1 Violation of the second Eliassen-Palm theorem
- 3.4 Quasi-biennial oscillation (1)
- 3.4 Quasi-biennial oscillation (2)
- Excercise (1)
- Excercise (2)
- Chapter 4 Rossby waves - 4.1 Shallow water equations (1)
- 4.1 Shallow water equations (2)
- 4.1 Shallow water equations (3)
- 4.2 Rossby waves (1)
- 4.2 Rossby waves (2)
- 4.2 Rossby waves (3)
- 4.2.1 Planetary scale internal stationary waves
- 4.2.2 Free oscillations
- 4.3 Remark on Kelvin waves: The case of v' = 0. (1)
- 4.3 Remark on Kelvin waves: The case of v' = 0. (2)
- Exercises
- Chapter 5 Vorticity and quasi-geostrophy - 5.1 Preliminary remarks - 5.1.1 Interpretation of vorticity (1)
- 5.1.1 Interpretation of vorticity (2)
- 5.2 Vorticity in the shallow water equations (1)
- 5.2 Vorticity in the shallow water equations (2)
- 5.2.1 Filtered Rossby waves (1)
- 5.2.1 Filtered Rossby waves (2)
- 5.3 Quasi-geostrophic shallow water theory (1)
- 5.3 Quasi-geostrophic shallow water theory (2)
- 5.3 Quasi-geostrophic shallow water theory (3)
- 5.3.1 Rossby radius / 5.3.2 Rossby number expansion (1)
- 5.3.2 Rossby number expansion (2)
- 5.4 Quasi-geostrophy in a stratified, compressible atmosphere (1)
- 5.4 Quasi-geostrophy in a stratified, compressible atmosphere (2)
- 5.4 Quasi-geostrophy in a stratified, compressible atmosphere (3)
- 5.4.1 Pseudo potential vorticity
- Exercises
- Chapter 6 The generation of eddies by instability - 6.1 Remarks
- 6.2 Instability
- 6.2.1 Buoyant convection
- 6.2.2 Rayleigh.Benard instability
- 6.2.3 Convective adjustment and gravity wave breaking
- 6.2.4 Reversal of mesopause temperature gradient / 6.2.5 Kelvin-Helmholtz instability (1)
- 6.2.5 Kelvin-Helmholtz instability (2)
- 6.2.6 Radiating and growing solutions
- 6.3 Instability of meteorological disturbances; baroclinic and barotropic instability (1)
- 6.3 Instability of meteorological disturbances; baroclinic and barotropic instability (2)
- 6.3 Instability of meteorological disturbances; baroclinic and barotropic instability (3)
- 6.3.1 A necessary condition for instability (1)
- 6.3.1 A necessary condition for instability (2)
- 6.3.1 A necessary condition for instability (3)
- 6.4 The Kelvin-Orr mechanism (1)
- 6.4 The Kelvin-Orr mechanism (2)
- 6.4 The Kelvin-Orr mechanism (3)
- 6.4 The Kelvin-Orr mechanism (4)
- 6.4 The Kelvin-Orr mechanism (5)
- 6.5 Two-level baroclinic model (1)
- RealPlayer is need for listening our video. it can be downloaded from RealNetworks Inc.