Dynamics of mixed bottom boundary layers and its implications for diapycnal transport in a stratified, natural water basin

Here we report on two field experiments from Lake Alpnach (surface area: 4. 8 km(2); maximum depth: 34 m) that were designed to study the process of bo undary mixing and to estimate its efficiency, the ratio between the turbule nt kinetic energy converted into potential energy and dissipated into heat, for diapycnal tracer transport. Lake Alpnach is particularly suited for th is purpose because it is known from earlier experiments that (1) its curren ts follow a regular oscillatory pattern, associated with basin-wide standin g internal waves (seiches, period similar to 0.5 days and 1 day, respective ly), and (2) diapycnal tracer transport is mainly caused by boundary mixing . During one of the experiments reported here, strong seiches were excited regularly and damped on a timescale of the order of 3 days; during the othe r experiment seiching motion was comparably weak. If seiching is excited re gularly, we find a persistent well-mixed bottom layer of 4-5 m height at th e deepest part of the lake. In the absence of regular seiching the layer di sappears within 10-20 days. On the sloping bottom boundaries the well-mixed layers (1) are of much more transient nature, (2) exhibit different therma l structure, and (3) decrease in thickness toward shallower depth inversely proportionally to the stability at the same depth in the lake interior. Th eir reduced thickness is possibly the result of repeatedly occurring intrus ions of boundary mixed water masses that are observed to extend horizontall y similar to 100-200 m into the lake interior. As a consequence of repeated generation of intrusions, mixing on the sloping boundaries is expected to be considerably more efficient compared to mixing over flat bottom boundari es. The observed mixing efficiency, the ratio of the rate of change of pote ntial energy below depth z caused by turbulence to the energy loss by botto m friction below depth z, increases indeed from 0.01 +/- 0.01 in the deepes t well-mixed layers to 0.15 +/- 0.04 in the upper pycnocline.