In this paper we solve two initial value problems for two-dimensional internal gravity waves. The waves are contained in a uniformly stratified, square-shaped domain whose sidewalls are tilted with respect to the direction of gravity. We consider several disturbances of the initial stream function field and solve both for its free evolution and for its evolution under parametric excitation. We do this by developing a structure-preserving numerical method for internal gravity waves in a two-dimensional stratified fluid domain. We recall the linearized, inviscid Euler-Boussinesq model, identify its Hamiltonian structure, and derive a staggered finite difference scheme that preserves this structure. For the discretized model, the initial condi...
A question of paramount importance in the dynamics of oceans is related to the energy cascade from l...
A question of paramount importance in the dynamics of oceans is related to the energy cascade from l...
It is well-known that internal wave breaking is the principle cause of ocean mixing. The latter play...
In this paper we solve two initial value problems for two-dimensional internal gravity waves. The wa...
Stratified fluids support internal waves, which propagate obliquely through the fluid. The angle w...
This paper gives background information for the fluid dynamics video on internal wave motion in a tr...
International audienceWe present a laboratory study on the instability of internal wave attractors i...
International audienceInternal gravity waves are propagating disturbances in stably stratified fluid...
In this second Chapter, we recall some basic notions on stably-stratified flows before focusing on i...
Abstract. Reflecting internal gravity waves in a stratified fluid preserve their frequency and thus ...
Time harmonic inviscid internal wave motions constrained to fully closed domains generically lead to...
International audienceTime harmonic inviscid internal wave motions constrained to fully closed domai...
Continuously stratified fluids support internal waves. The energy of these waves propagates under an...
International audienceThe Boussinesq approximation provides a convenient framework to describe the d...
A question of paramount importance in the dynamics of oceans is related to the energy cascade from l...
A question of paramount importance in the dynamics of oceans is related to the energy cascade from l...
A question of paramount importance in the dynamics of oceans is related to the energy cascade from l...
It is well-known that internal wave breaking is the principle cause of ocean mixing. The latter play...
In this paper we solve two initial value problems for two-dimensional internal gravity waves. The wa...
Stratified fluids support internal waves, which propagate obliquely through the fluid. The angle w...
This paper gives background information for the fluid dynamics video on internal wave motion in a tr...
International audienceWe present a laboratory study on the instability of internal wave attractors i...
International audienceInternal gravity waves are propagating disturbances in stably stratified fluid...
In this second Chapter, we recall some basic notions on stably-stratified flows before focusing on i...
Abstract. Reflecting internal gravity waves in a stratified fluid preserve their frequency and thus ...
Time harmonic inviscid internal wave motions constrained to fully closed domains generically lead to...
International audienceTime harmonic inviscid internal wave motions constrained to fully closed domai...
Continuously stratified fluids support internal waves. The energy of these waves propagates under an...
International audienceThe Boussinesq approximation provides a convenient framework to describe the d...
A question of paramount importance in the dynamics of oceans is related to the energy cascade from l...
A question of paramount importance in the dynamics of oceans is related to the energy cascade from l...
A question of paramount importance in the dynamics of oceans is related to the energy cascade from l...
It is well-known that internal wave breaking is the principle cause of ocean mixing. The latter play...