Research

My primary research focus lies in the application of advanced numerical methods and algorithms to address fluid dynamics problems, including but not limited to global spectral methods, spectral-element methods, and optimisation techniques. I am particularly drawn to the intricate nature of geophysical, astrophysical, and industrial fluid flows, which demand a high degree of freedom for accurate solutions. To tackle these challenges, I leverage the power of high-performance computing, a vital tool in the current scientific paradigm.

Small-scale properties of buoyancy-driven turbulence

As a doctoral student at the Indian Institute of Technology (IIT) Kanpur, my research focused on understanding the dynamics of buoyancy-driven turbulent flows by means of direct numerical simulations (DNS). Flows driven by buoyancy can be classified into two categories. First, convective flows in which hotter and lighter fluid at the bottom rises, while colder and heavier fluid at the top comes down. This situation is represented in figure (a), where the temperature isosurfaces exhibit ascending hot plumes (red) and descending cold plumes (blue). Second is stably stratified flow, in which lighter fluid rests above heavier fluid (see figure (b)).

(a) Convective turbulence exhibits ascending hot plumes (red) and descending cold plumes (blue) (Kumar & Verma, 2018).

(b) A density plot of the temperature field for stably stratified turbulence was calculated at a grid resolution of 8192^2 points (Kumar et al., 2017).

(c) Kinetic energy spectrum E(k) as a function of wavenumber k computed for convective turbulence at 4096^3 grid points (Verma et al., 2017).

More precisely, my work focused on the quantification of small-scale quantities for stably stratified turbulence (SST) and convective turbulence, for which I was involved in developing the global spectral code TARANG (Chatterjee et al., 2017)  and the finite-volume code OpenFOAM (Kumar & Verma, 2018). An important unsolved problem in the field of buoyancy-driven turbulence is how to quantify the spectra and fluxes of kinetic and potential energies. Using high-resolution DNS, performed at a grid resolution of $4096^3$ in a cubical box, we have shown a delicate balance of dissipation and energy supply rate by buoyancy (Kumar et al., 2014; Verma et al., 2017). This balance leads to a constant kinetic energy (KE) flux, and therefore, we observe Kolmogorov’s spectrum exhibited in figure (c). On the other hand, at moderate stratification for stably stratified turbulent flows, we have shown that the energy supply rate by buoyancy is negative, which indicates the conversion of kinetic energy to potential energy by buoyancy; thus, the KE flux decreases with wavenumber (Kumar et al., 2017). As a result, the system exhibits Bolgiano-Obukhov (BO) scaling. Further, we have confirmed these scaling results by applying the low-dimensional shell model (Kumar & Verma, 2015).

Investigating instabilities in mixed baroclinic convection in a cavity

In this study, we investigated the convective patterns that develop in a nearly semicylindrical cavity. This cavity is supplied with hot fluid at the top boundary and has a cold, porous semicircular boundary at the bottom, extending infinitely in the third dimension (see figure (a)). While this setup is pertinent to the more intricate continuous casting processes, our focus is on the flow patterns resulting from the specific type of mixed convection present in this configuration. We employed linear stability analysis (LSA) and direct numerical simulations (DNS), utilising the spectral-element code Nektar++ to identify observable states. Additionally, the nature of the bifurcations was characterised through Stuart–Landau analysis. For more details, see our paper (Kumar & Potherat, 2020).

(a) Two-dimensional base flow obtained through DNS. Here colours represent the temperature field and arrows represent the velocity vector.

(b) Critical Rayleigh number (Ra_c) as a function of Reynolds number (Re). Blue (orange) regions below (above) the curve represents flow regimes that are linearly stable (unstable) to two or three-dimensional perturbations.