Small-scale turbulence and vertical mixing in Lake Baikal

The water column of Lake Baikal is extremely weakly-but permanently-stratif ied below 250 m. Despite the thickness of this relatively stagnant water ma ss of more than 1000 m, the water age (time since last contact with the atm osphere) is only slightly more than a decade, indicating large-scale advect ive exchange. In the stratified deep water, the fate of water constituents is determined by the combined action of advective processes (deep-water int rusions) and small-scale turbulent vertical diffusion. Here, vertical diffu sivity is addressed through the analysis of 25 temperature microstructure p rofiles collected in the three major basins of Lake Baikal to a depth of 60 0 m. In addition, in the 1,432-m deep south basin, monthly CTD profiles and a two year record of near-bottom currents were analyzed. Balancing turbule nt kinetic energy and small-scale temperature variance leads to the conclus ions that (1) vertical diffusivity in the stratified deep water ranges from 10-90 X 10(-4) m(2) s(-1) (between 600 and 250 m), which is three orders o f magnitude more than estimated by Killworth et al. (1996), (2) the mixing efficiency is similar to 0.16, comparable to that found in stronger stratif ication (e.g., the ocean interior), (3) turbulence under ice decays with a time scale of 40 +/- 2 d and (4) the interior of the permanently stratified deep water below 250 m and the bottom boundary layer contribute roughly eq ually to the TKE production. The latter implies, that mixing in the deep wa ter of Lake Baikal's three sub-basins is dominated by bottom boundary mixin g as found in smaller lakes and ocean basins.