湍黏系数对浅滩海域三维风暴潮的影响
Effects of turbulent viscosity coefficient on 3-D storm surge within shallow seas
-
摘要: 利用WRF大气模式和基于有限体积法的三维海洋数值模型FVCOM,建立了连云港及其附近浅滩海域的三维风暴潮流数学模型。运用k-ε和MY-2.5两种不同的湍流模型,对“韦帕”台风作用下的三维风暴潮流进行了数值模拟,并对计算得到的三维风暴潮流流场结果和垂向湍流黏性系数结果进行了对比分析。计算分析结果表明,两种不同湍流模型计算所得的风暴潮增水差别很小,可以忽略;但在风生流较强的时间段内,MY-2.5湍流模型计算所得的水平流速流向沿垂向分布并不一致,而k-ε湍流模型的计算结果较好,与实测分层潮流资料更为符合。研究结果表明,垂向湍流黏性系数沿水深的垂向分布对浅滩海域风暴潮流水平流速的垂向结构至关重要,建议选用k-ε湍流模型计算垂向湍流黏性系数和湍流扩散系数。Abstract: Using a WRF atmospheric model and a 3-D ocean numerical model FVCOM based on finite volume method, a three-dimensional numerical model of storm surge within Lianyungang shallow waters is developed. The 3-D storm surge during typhoon WIPHA is simulated by use of different turbulence models such as k-ε and MY-2.5. The simulation results of the 3-D storm surge flow and vertical turbulence viscosity coefficient are analyzed in the study. The analysis results show that, compared with the poor results from MY-2.5 model, the vertical velocity and direction distribution of the storm surge calculated by k-ε model has a good agreement with the measured data, and the values of the vertical turbulence viscosity coefficient are crucial for the vertical structure of the storm surge, therefore a right turbulence model is preferred. The k-ε turbulence model is suggested for simulation of the 3-D storm surge in the future.