By solving the linear quasi-geostrophic set of equations pertinent to the Eady model, the complex eigenvalues and the eigenfunctions are obtained. The propagation speed and the growth rate are computed. Quantitative information is provided about the wave structures for several unstable models, a marginally stable mode, and a stable mode. The peculiarities concerning the amplitude and the phase variations of the waves are noted as the wavenumber varies from the unstable region to the stable region. Physical interpretations of the interrelationships among the dynamical variables are given, with a view toward revealing important aspects of the energy transfer from the basic state to the growing waves
A theoretical framework is developed for the evolution of baroclinic waves with latent heat release ...
The downstream development in both space and time of baroclinic instability is studied in a nonlinea...
Baroclinic instability, the fundamental mechanism underlying the generation of baroclinic eddies in...
A numerical investigation of baroclinic instability of nongeostrophic wave perturbations with differ...
An aquaplanet model is used to study the nature of the highly persistent low-frequency waves that ha...
The research carried out in the past year dealt with nonlinear baroclinic wave dynamics. The model c...
An aquaplanet model is used to study the nature of the highly persistent low-frequency waves that ha...
Two main areas of theoretical research in geophysical fluid dynamics---linearized instability and no...
Baroclinic instability of zonally forced flow in a two mode quasi-geostrophic numerical model with p...
Wavenumber transition and hysteresis in a highly unstable baroclinic flow are investigated using a h...
Completed and ongoing research activities are discussed briefly, including a three-dimensional, line...
The evolution of atmospheric baroclinic waves is investigated by a six-layer forced dissipative quas...
Here, we explore the transition from symmetric instability to ageostrophic baroclinic instability in...
A nonlinear stability theorem is established for Eady's model of baroclinic flow. In particular, the...
Linear stability analyses are performed on a wide range of mean flows simulated with a dry idealized...
A theoretical framework is developed for the evolution of baroclinic waves with latent heat release ...
The downstream development in both space and time of baroclinic instability is studied in a nonlinea...
Baroclinic instability, the fundamental mechanism underlying the generation of baroclinic eddies in...
A numerical investigation of baroclinic instability of nongeostrophic wave perturbations with differ...
An aquaplanet model is used to study the nature of the highly persistent low-frequency waves that ha...
The research carried out in the past year dealt with nonlinear baroclinic wave dynamics. The model c...
An aquaplanet model is used to study the nature of the highly persistent low-frequency waves that ha...
Two main areas of theoretical research in geophysical fluid dynamics---linearized instability and no...
Baroclinic instability of zonally forced flow in a two mode quasi-geostrophic numerical model with p...
Wavenumber transition and hysteresis in a highly unstable baroclinic flow are investigated using a h...
Completed and ongoing research activities are discussed briefly, including a three-dimensional, line...
The evolution of atmospheric baroclinic waves is investigated by a six-layer forced dissipative quas...
Here, we explore the transition from symmetric instability to ageostrophic baroclinic instability in...
A nonlinear stability theorem is established for Eady's model of baroclinic flow. In particular, the...
Linear stability analyses are performed on a wide range of mean flows simulated with a dry idealized...
A theoretical framework is developed for the evolution of baroclinic waves with latent heat release ...
The downstream development in both space and time of baroclinic instability is studied in a nonlinea...
Baroclinic instability, the fundamental mechanism underlying the generation of baroclinic eddies in...