We perform the stability analysis for a free surface fluid current modeled as two finite layers of constant vorticity, under the action of gravity and absence of surface tension. In the same spirit as Taylor ["Effect of variation in density on the stability of superposed streams of fluid," Proc. R. Soc. A 132, 499 (1931)], a geometrical approach to the problem is proposed, which allows us to present simple analytical criteria under which the flow is stable. A strong destabilizing effect of stratification in density is revealed by comparison with the physical setting where the vorticity interface is also a density interface separating two immiscible fluids with constant densities
The problem of two layers of immiscible fluid, bordered above by an unbounded layer of passive fluid...
In homogeneous and density-stratified inviscid shear flows, the mechanism for instability that is mo...
We investigate the linear stability of zonal shear flows with a free surface (like the flow in ocean...
We perform the stability analysis for a free surface fluid current modeled as two finite layers of c...
We perform the stability analysis for a free surface fluid current modeled as two finite layers of c...
Stern & Adam and subsequent workers have considered the linear stability of two-dimensional, parall...
Stern & Adam and subsequent workers have considered the linear stability of two-dimensional, parall...
In this paper, we first revisit the celebrated Boussinesq approximation in stratified flows. Using s...
In this paper, we first revisit the celebrated Boussinesq approximation in stratified flows. Using s...
In this paper, we have considered the effects of the shallowness of the domain as well as the air-wa...
In this paper, we have considered the effects of the shallowness of the domain as well as the air-wa...
We revisit the stability analysis for three classical configurations of multiple fluid layers propos...
The stability of a mixing layer made up of two miscible fluids, with a viscosity-stratified layer be...
Both surface tension and buoyancy force in stable stratification act to restore perturbed interfaces...
We investigate the linear stability of zonal shear flows with a free surface (like the flow in ocean...
The problem of two layers of immiscible fluid, bordered above by an unbounded layer of passive fluid...
In homogeneous and density-stratified inviscid shear flows, the mechanism for instability that is mo...
We investigate the linear stability of zonal shear flows with a free surface (like the flow in ocean...
We perform the stability analysis for a free surface fluid current modeled as two finite layers of c...
We perform the stability analysis for a free surface fluid current modeled as two finite layers of c...
Stern & Adam and subsequent workers have considered the linear stability of two-dimensional, parall...
Stern & Adam and subsequent workers have considered the linear stability of two-dimensional, parall...
In this paper, we first revisit the celebrated Boussinesq approximation in stratified flows. Using s...
In this paper, we first revisit the celebrated Boussinesq approximation in stratified flows. Using s...
In this paper, we have considered the effects of the shallowness of the domain as well as the air-wa...
In this paper, we have considered the effects of the shallowness of the domain as well as the air-wa...
We revisit the stability analysis for three classical configurations of multiple fluid layers propos...
The stability of a mixing layer made up of two miscible fluids, with a viscosity-stratified layer be...
Both surface tension and buoyancy force in stable stratification act to restore perturbed interfaces...
We investigate the linear stability of zonal shear flows with a free surface (like the flow in ocean...
The problem of two layers of immiscible fluid, bordered above by an unbounded layer of passive fluid...
In homogeneous and density-stratified inviscid shear flows, the mechanism for instability that is mo...
We investigate the linear stability of zonal shear flows with a free surface (like the flow in ocean...