Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Effect of Wind Stress on Stratified Deep Lake
The basic equations for wind-driven flows in deep two-layered lakes are outlined. The deepening of the upper layer due to entrainment of more dense water from the lower layer is explained physically, and the entrainment is then related to the wind shear stress at the water surface and an overall Richardson number. The general shapes of the distributions of shear stress and velocity are outlined. Diffusion and dispersion coefficients are calculated and related to the depth of the upper layer and to the wind shear stress at the surface.
Effect of Wind Stress on Stratified Deep Lake
The basic equations for wind-driven flows in deep two-layered lakes are outlined. The deepening of the upper layer due to entrainment of more dense water from the lower layer is explained physically, and the entrainment is then related to the wind shear stress at the water surface and an overall Richardson number. The general shapes of the distributions of shear stress and velocity are outlined. Diffusion and dispersion coefficients are calculated and related to the depth of the upper layer and to the wind shear stress at the surface.
Effect of Wind Stress on Stratified Deep Lake
Hansen, Niels-Erik Ottesen (Autor:in)
Journal of the Hydraulics Division ; 101 ; 1037-1052
01.01.2021
161975-01-01 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Unbekannt
Wind stress over waves in stably stratified flow
| Online Contents | 1999
| British Library Online Contents | 2008
Effect of wind on highly stratified flow
| British Library Conference Proceedings | 2005