Fluid Mixing in Stratified Gravity Currents: The Prandtl Mixing Length

Shear-induced vertical mixing in a stratified flow is a key ingredient of thermohaline circulation. We experimentally determine the vertical flux of momentum and density of a forced gravity current using high-resolution velocity and density measurements. A constant eddy-viscosity model provides a poor description of the physics of mixing, but a Prandtl mixing length model relating momentum and density fluxes to mean velocity and density gradients works well. For the average gradient Richardson number Ri₆0. 08 and a Taylor Reynolds number Re_100, the mixing lengths are fairly constant, about the same magnitude, comparable to the turbulent shear length.