It is shown that the influence of topography on the interaction of long, weakly nonlinear, quasigeostrophic baroclinic waves can be described by a pair of linearly coupled Korteweg–de Vries equations, with a forcing term in one of the equations. This system exhibits a rich dynamics that is suggestive of atmospheric blocking such as stable stationary solutions, transient quasi-steady-state solutions, multiple equilibria, and baroclinic instability. Topography is shown to favor the formation of blocking systems. This system is investigated both analytically, using techniques from asymptotic perturbation theory, and through numerical simulations. 1
In a preceding paper the authors showed that planetary waves of very different amplitudes can be sus...
The research carried out in the past year dealt with nonlinear baroclinic wave dynamics. The model c...
In a preceding paper the authors showed that planetary waves of very different amplitudes can be sus...
It is shown that the interaction of long, weakly nonlinear, quasigeostrophic baroclinic waves can be...
The local linear stability of forced, stationary long waves produced by topography or potential vort...
Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Meteorology and Physical Oceanograph...
Stationary flow of a barotropic fluid in a β channel has been shown by Charney and De Vore (1979) to...
Stationary flow of a barotropic fluid in a β channel has been shown by Charney and De Vore (1979) to...
Stationary flow of a barotropic fluid in a β channel has been shown by Charney and De Vore (1979) to...
(Manuscript received November 10,1975; in fmal form March 2,1976) A two-level, b-plane, quasi-geostr...
While not as widely discussed as long wave soliton models of atmospheric and oceanic phenomena envel...
While not as widely discussed as long wave soliton models of atmospheric and oceanic phenomena envel...
It is well established that forced planetary waves are critically important for blocking formation. ...
The stability of free and forced planetary waves in a $ beta$-channel is investigated with a barotro...
The evolution of atmospheric baroclinic waves is investigated by a six-layer forced dissipative quas...
In a preceding paper the authors showed that planetary waves of very different amplitudes can be sus...
The research carried out in the past year dealt with nonlinear baroclinic wave dynamics. The model c...
In a preceding paper the authors showed that planetary waves of very different amplitudes can be sus...
It is shown that the interaction of long, weakly nonlinear, quasigeostrophic baroclinic waves can be...
The local linear stability of forced, stationary long waves produced by topography or potential vort...
Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Meteorology and Physical Oceanograph...
Stationary flow of a barotropic fluid in a β channel has been shown by Charney and De Vore (1979) to...
Stationary flow of a barotropic fluid in a β channel has been shown by Charney and De Vore (1979) to...
Stationary flow of a barotropic fluid in a β channel has been shown by Charney and De Vore (1979) to...
(Manuscript received November 10,1975; in fmal form March 2,1976) A two-level, b-plane, quasi-geostr...
While not as widely discussed as long wave soliton models of atmospheric and oceanic phenomena envel...
While not as widely discussed as long wave soliton models of atmospheric and oceanic phenomena envel...
It is well established that forced planetary waves are critically important for blocking formation. ...
The stability of free and forced planetary waves in a $ beta$-channel is investigated with a barotro...
The evolution of atmospheric baroclinic waves is investigated by a six-layer forced dissipative quas...
In a preceding paper the authors showed that planetary waves of very different amplitudes can be sus...
The research carried out in the past year dealt with nonlinear baroclinic wave dynamics. The model c...
In a preceding paper the authors showed that planetary waves of very different amplitudes can be sus...