International audienceDirect numerical simulation is used to study the air flow between two vertical plates maintained at different temperatures. The periodic dimensions of the plates are small so as to accommodate only one flow structure, which consists of a convection roll with oblique vorticity braids. At lower Rayleigh numbers, the roll and the braids grow and shrink alternatively following a cyclical process. As the Rayleigh number is increased, the flow becomes temporally chaotic through a period-doubling cascade. Windows corresponding to multiperiodic regimes and interior crises are observed. As the Rayleigh number is further increased, the structure intermittently switches between two vertical positions, which is seen to correspond ...
Natural convection ows arising from a horizontal cylinder centred ina square-sectioned enclosure are...
We report experiments on thermally driven convection in an inclined layer of large aspect ratio in a...
Double-diffusive convection in a horizontally infinite layer of a unit height in a large Rayleigh nu...
Direct numerical simulation is used to study the air flow between two vertical plates maintained at ...
International audienceNatural convection of air between two infinite vertical differentially heated ...
National audienceThe chaotic regime of the natural convection of air between two vertical plates mai...
International audienceThe transition to the chaos of the air flow between two vertical plates mainta...
The aim of the present study is the analysis of the transition to turbulence of natural convection f...
Aim of the present study is the preliminary numerical analysis of the transition to turbulence of na...
Bifurcating thermal convection flows arising from a horizontal cylinder centred in a square-sectione...
Convective flows of a small Prandtl number fluid contained in a two dimensional cavity subject to a ...
Convective flows of a small Prandtl number fluid contained in a two-dimensional cavity subject to a ...
A theoretical study is presented of convection in a horizontal fluid layer heated from below or abov...
La transition vers le chaos de la convection naturelle d air entre deux plaques infinies verticales ...
The sequence of bifurcations leading to the onset of chaotic flow is determined numerically, for the...
Natural convection ows arising from a horizontal cylinder centred ina square-sectioned enclosure are...
We report experiments on thermally driven convection in an inclined layer of large aspect ratio in a...
Double-diffusive convection in a horizontally infinite layer of a unit height in a large Rayleigh nu...
Direct numerical simulation is used to study the air flow between two vertical plates maintained at ...
International audienceNatural convection of air between two infinite vertical differentially heated ...
National audienceThe chaotic regime of the natural convection of air between two vertical plates mai...
International audienceThe transition to the chaos of the air flow between two vertical plates mainta...
The aim of the present study is the analysis of the transition to turbulence of natural convection f...
Aim of the present study is the preliminary numerical analysis of the transition to turbulence of na...
Bifurcating thermal convection flows arising from a horizontal cylinder centred in a square-sectione...
Convective flows of a small Prandtl number fluid contained in a two dimensional cavity subject to a ...
Convective flows of a small Prandtl number fluid contained in a two-dimensional cavity subject to a ...
A theoretical study is presented of convection in a horizontal fluid layer heated from below or abov...
La transition vers le chaos de la convection naturelle d air entre deux plaques infinies verticales ...
The sequence of bifurcations leading to the onset of chaotic flow is determined numerically, for the...
Natural convection ows arising from a horizontal cylinder centred ina square-sectioned enclosure are...
We report experiments on thermally driven convection in an inclined layer of large aspect ratio in a...
Double-diffusive convection in a horizontally infinite layer of a unit height in a large Rayleigh nu...