Using Different Classic Turbulence Closure Models to Assess Salt and Temperature Modelling in a Lagunar System: A Sensitivity Study

被引:1
作者
Lopes, Jose Fortes [1 ]
机构
[1] Univ Aveiro, Dept Fis, CESAM, P-3810193 Aveiro, Portugal
关键词
Ria de Aveiro lagoon; turbulence models; k-epsilon; Smagorinsky; eddy viscosity; salinity; temperature; LARGE-EDDY SIMULATIONS; RIA-DE-AVEIRO; PERFORMANCE; PREDICTION; UNCERTAINTY; SALINITY; LAYER;
D O I
10.3390/jmse10111750
中图分类号
U6 [水路运输]; P75 [海洋工程];
学科分类号
0814 ; 081505 ; 0824 ; 082401 ;
摘要
Turbulence modelling is an important issue when dealing with hydrodynamic and transport models for better simulation of the transport of dissolved or suspended substances in a body-water. It controls processes involving physical balances (salt and water temperature) and, therefore, the ecosystem equilibrium. The study arises from the need to model the turbulence more efficiently when dealing with extreme situations on the Ria de Aveiro (Portugal), a coastal lagoon shallow water system dominated by tidal transport. Because the turbulence model is coupled to the hydrodynamic and transport models, a correct estimation of the eddy viscosity is important in simulating the salt and the heat transports. The aim is to assess the performance of four turbulence schemes/models (k, k-epsilon, Smagorinsky's, and k-epsilon/Smagorinsky's (k-epsilon/Sma), where k is turbulent kinetic energy and epsilon the dissipation rate of the turbulent kinetic energy) associated to a coupled hydrodynamic and transport models to simulate the eddy viscosity, the salinity, and the temperature. Overall, the results point out that among the different models/schemes used, the is the one which provides a more realistic value of the eddy viscosity within the range (1-6) m(2) s(-1), but most probably (1-3) m(2) s(-1). The application of the sensitivity analysis to some non-universal k-epsilon/Sma parameters evidenced significant sensitivity for the eddy viscosity and the salinity and moderate sensitivity for the water temperature. A 100% adjustment of the parameter values relative to the reference, translated into variations within the range of (1, 4) m(2) s(-1), (0, 13) PSU, and (1, 2.20) & DEG;C, for the eddy viscosity, salinity, and water temperature, respectively.
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页数:25
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