| Автор | Wüest, Alfred |
| Автор | Lorke, Andreas |
| Дата выпуска | 2003 |
| dc.description | ▪ Abstract Recent small-scale turbulence observations allow the mixing regimes in lakes, reservoirs, and other enclosed basins to be categorized into the turbulent surface and bottom boundary layers as well as the comparably quiet interior. The surface layer consists of an energetic wave-affected thin zone at the very top and a law-of-the-wall layer right below, where the classical logarithmic-layer characteristic applies on average. Short-term current and dissipation profiles, however, deviate strongly from any steady state. In contrast, the quasi-steady bottom boundary layer behaves almost perfectly as a logarithmic layer, although periodic seiching modifies the structure in the details. The interior stratified turbulence is extremely weak, even though much of the mechanical energy is contained in baroclinic basin-scale seiching and Kelvin waves or inertial currents (large lakes). The transformation of large-scale motions to turbulence occurs mainly in the bottom boundary and not in the interior, where the local shear remains weak and the Richardson numbers are generally large. |
| Формат | application.pdf |
| Издатель | Annual Reviews |
| Копирайт | Annual Reviews |
| Название | SMALL-SCALE HYDRODYNAMICS IN LAKES |
| DOI | 10.1146/annurev.fluid.35.101101.161220 |
| Print ISSN | 0066-4189 |
| Журнал | Annual Review of Fluid Mechanics |
| Том | 35 |
| Первая страница | 373 |
| Последняя страница | 412 |
| Аффилиация | Wüest, Alfred; Applied Aquatic Ecology (APEC), Limnological Research Center, EAWAG, Kastanienbaum, Switzerland; email: alfred.wuest@eawag.ch andreas.lorke@eawag.ch |
