Advances in Water Resources and Hydraulic Engineering 2009
DOI: 10.1007/978-3-540-89465-0_125
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Numerical Simulation of Hydrodynamic Characteristics and Water Quality in Yangchenghu Lake

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Cited by 7 publications
(9 citation statements)
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“…The second comparison was done with a study of Nam Theun 2 reservoir, a large and shallow reservoir of 506 km 2 , mean depth of 8 m and maximum depth of 35 m in Lao PDR [6]. The third comparison was done with a study of Lake Yangchenghu, a large and shallow lake of 118 km 2 in China, composed of three basins whose the mean depth are 1.7, 1.8, and 2.65 m [7]. We compared the model configuration between these three study sites and Lake Créteil (Tables 1and 2): (i) the turbulence model: background horizontal eddy viscosity, background horizontal eddy diffusivity of heat, background vertical eddy viscosity, background vertical eddy diffusivity of heat, Ozmidov length; (ii) the flow boundary conditions: wind drag coefficient; and (iii) the heat flux model: Dalton number, Stanton number, and coefficient for free convection.…”
Section: Calibration Parametersmentioning
confidence: 99%
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“…The second comparison was done with a study of Nam Theun 2 reservoir, a large and shallow reservoir of 506 km 2 , mean depth of 8 m and maximum depth of 35 m in Lao PDR [6]. The third comparison was done with a study of Lake Yangchenghu, a large and shallow lake of 118 km 2 in China, composed of three basins whose the mean depth are 1.7, 1.8, and 2.65 m [7]. We compared the model configuration between these three study sites and Lake Créteil (Tables 1and 2): (i) the turbulence model: background horizontal eddy viscosity, background horizontal eddy diffusivity of heat, background vertical eddy viscosity, background vertical eddy diffusivity of heat, Ozmidov length; (ii) the flow boundary conditions: wind drag coefficient; and (iii) the heat flux model: Dalton number, Stanton number, and coefficient for free convection.…”
Section: Calibration Parametersmentioning
confidence: 99%
“…In Lake Créteil, the fetch length is not such that large surface waves can form and increase the wind drag coefficient. The wind drag coefficient was set to 0.0005 for Nam Theun 2 reservoir [6] and 0.0025 for Lake Yangchenghu [7]. This coefficient depends on the type of wind record and on the location of the meteorological station where wind speed was recorded.…”
Section: Calibration Parametersmentioning
confidence: 99%
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“…Zhu et al [1] not only simulated currents from three dimensional hydrodynamic characte-ristics but also employed a two-dimensional water quality numerical model to simulate diffusion and transport of pollutants in Lake Yangchenghu. You et al [2] investigated eutrophication in Lake Taihu by simulating the effects of hydrodynamics on phosphorus fluxes.…”
Section: Introductionmentioning
confidence: 99%