arXiv subjects

Lima Biswas

Publications and source records attributed to Lima Biswas.

3 recordsLinked to original sources

arXiv2025

Stability analysis of time-periodic shear flow generated by an oscillating density interface

We consider the conceptual two-layered oscillating tank of Inoue & Smyth (2009), which mimics the time-periodic parallel shear flow generated by low-frequency (e.g. semi-diurnal tides) and small-angle oscillations of the density interface. Such self-induced shear of an oscillating pycnocline may provide an alternate pathway to pycnocline turbulence and diapycnal mixing in addition to the turbulence and mixing driven by wind-induced shear of the surface mixed layer. We theoretically investigate shear instabilities arising in the inviscid two-layered oscillating tank configuration and show that the equation governing the evolution of linear perturbations on the density interface is a Schr\"odinger-type ordinary differential equation with a periodic potential. The necessary and sufficient stability condition is governed by a nondimensional parameter $\beta$ resembling the inverse Richardson number; for two layers of equal thickness, instability arises when $\beta\!>\!1/4$. When this condition is satisfied, the flow is initially stable but finally tunnels into the unstable region after reaching the time marking the turning point. Once unstable, perturbations grow exponentially and reveal characteristics of Kelvin-Helmholtz (KH) instability. The Modified Airy Function method, which is an improved variant of the Wentzel-Kramers-Brillouin (WKB) theory, is implemented to obtain a uniformly valid, composite approximate solution to the interface evolution. Next, we analyse the fully nonlinear stages of interface evolution by modifying the circulation evolution equation in the standard vortex blob method, which reveals that the interface rolls up into KH billows. Finally, we undertake real case studies of Lake Geneva and Chesapeake Bay to provide a physical perspective.

physics.flu-dyn↗

arXiv2021

Resonant triad interactions in stably-stratified uniform shear flow

We investigate exact and near resonant triad interactions (RTI) in a two-dimensional stably stratified uniform shear flow confined between two infinite parallel walls in the absence of viscous and diffusive effects. RTI occur when three interacting waves satisfy the resonance conditions of the form $k_1 \pm k_2 = k_3$ and $ω_1 \pm ω_2 = ω_3$ with $k_i$ and $ω_i$ being the wavenumber and frequency of the ith wave ($i \in {1,2,3}$), respectively. The linear stability problem is solved analytically, which gives the eigenfunctions in the form of the modified Bessel functions. It is identified that an interaction between two primary modes having the same frequency $ω$ but different wavenumbers $k_m$ and $k_n$ produces two different secondary modes: one time-dependent (superharmonic) mode having frequency $2ω$ and wavenumber $k_m +k_n$, and the other time-independent (subharmonic) mode with $ω= 0$ and wavenumber $k_m - k_n$. The differential equation governing the spatial amplitude of the superharmonic mode is solved numerically as well as analytically using the method of variation of parameters. It turns out that the linear operator associated with the differential equation of the superharmonic mode is the same as the linear stability operator and that the solvability condition of the differential equation is found to be associated with the existence of RTI. The existence of resonant triad interactions predicted by the dispersion relation, are justified by showing the divergence of the spatial amplitude of superharmonic mode. Various cases of wave interactions in a stably stratified shear flow are analysed in the presence of a resonant triad for various frequencies and linear stratifications.

physics.flu-dyn↗

arXiv2019

Shear-banding instability in arbitrarily inelastic granular shear flows

One prototypical instability in granular flows is the shear-banding instability, in which a uniform granular shear flow breaks into alternating bands of dense and dilute clusters of particles having low and high shear (shear stress or shear rate), respectively. In this work, the shear-banding instability in an arbitrarily inelastic granular shear flow is analyzed through the linear stability analysis of granular hydrodynamic equations closed with Navier--Stokes-level constitutive relations. It is shown that the choice of appropriate constitutive relations plays an important role in predicting the shear-banding instability. A parametric study is carried out to study the effect of the restitution coefficient, channel width and mean density. Two global criteria relating the control parameters are found for the onset of the shear-banding instability.

cond-mat.soft↗