Energetics and mixing in buoyancy-driven near-bottom stratified flow

Turbulence and mixing in a near- bottom convectively driven flow are examined by numerical simulations of a model problem: a statically unstable disturbance at a slope with inclination fi in a stable background with buoyancy frequency N. The influence of slope angle and initial disturbance amplitude are quantified in a parametric study. The flow evolution involves energy exchange between four energy reservoirs, namely the mean and turbulent components of kinetic energy (KE) and available potential energy (APE). In contrast to the zero- slope case where the mean flow is negligible, the presence of a slope leads to a current that oscillates with !D N sin fi and qualitatively changes the subsequent evolution of the initial density disturbance. The frequency, N sin fi, and the initial speed of the current are predicted using linear theory. The energy transfer in the sloping cases is dominated by an oscillatory exchange between mean APE and mean KE with a transfer to turbulence at specific phases. In all simulated cases, the positive buoyancy flux during episodes of convective instability at the zero- velocity phase is the dominant contributor to turbulent kinetic energy (TKE) although the shear production becomes increasingly important with increasing fi. Energy that initially resides wholly in mean available potential energy is lost through conversion to turbulence and the subsequent dissipation of TKE and turbulent available potential energy. A key result is that, in contrast to the explosive loss of energy during the initial convective instability in the non- sloping case, the sloping cases exhibit a more gradual energy loss that is sustained over a long time interval. The slope- parallel oscillation introduces a new flow time scale T D 2 p=. N sin fi/ and, consequently, the fraction of initial APE that is converted to turbulence during convective instability progressively decreases with increasing fi. For moderate slopes with fi < 10 ffi, most of the net energy loss takes place during an initial, short (Nt 20) interval with periodic convective overturns. For steeper slopes, most of the energy loss takes place during a later, long (Nt > 100) interval when both shear and convective instability occur, and the energy loss rate is approximately constant. The mixing efficiency during the initial period dominated by convectively driven turbulence is found to be substantially higher (exceeds 0.5) than the widely used value of 0.2. The mixing efficiency at long time in the present problem of a convective overturn at a boundary varies between 0.24 and 0.3.