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A novel sigma coordinate system to simulate abrupt changes of underwater terrain in a hydrodynamic model: application to Lake Mead, USA

机译:一种新颖的Sigma坐标系,模拟水下地形中水下地形的突然变化:在美国湖米德的应用

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摘要

The sigma (SIG) coordinate system in ocean circulation simulation models results inevitably in horizontal pressure gradient error. This problem also emerges in models of deep lakes or reservoirs with the same characteristics of underwater terrain mutation. SIG coordinates reflect vertical relative stratification but cannot be used to calculate horizontal pressure gradient force in places with drastic topographic changes; this results in vertical water temperature and circulation errors. In deep lakes or reservoirs, differences in water density caused by the temperature difference between upper and lower water bodies is the primary cause of thermal stratification phenomena. Lake Mead was used as a case study on steep topography based on Environmental Fluid Dynamics Code (EFDC) model in this study. SIG coordinates result in close agreement between the calibrated temperature time series at the top and middle water layers, but disparity in the bottom water layer. The error emerges in the horizontal pressure gradient error due to the SIG coordinate transformation. Neither increasing the vertical resolution nor adjusting the horizontal viscosity coefficient resolve this error. We test the sigma-zed (SGZ) coordinate which combines Z coordinate and SIG coordinate as a replacement for the SIG coordinate to find that they effectively reduce the model’s runtime and simulation efficiency. The vertical temperature distribution in SGZ coordinate mode is more accurate than the distribution in SIG coordinate mode. The Navier-Stokes horizontal gradient and advection diffusion equation results under SIG coordinates are very sensitive to the pressure gradient. The replacement also enhances resolution near the thermocline, facilitates reclosing of the water bottom and the equal sigma surface, lends significant advantages in terms of vertical temperature in the simulation for local deep water with steep terrain, and shortens runtime for 0.14?h. SGZ mixed coordinates are recommended in the simulation of deep lakes or reservoirs wherein the underwater topography is large (with abundant continuous deep trenches or reefs).
机译:海洋循环仿真模型中的Sigma(SIG)坐标系会导致水平压力梯度误差导致误差。这种问题也出现在深湖泊或水库的模型中,具有相同的水下地形突变特征。 SIG坐标反映了垂直相对分层,但不能用于在具有剧烈地形变化的地方计算水平压力梯度力;这导致垂直水温和循环误差。在深湖泊或水库中,上下水体之间的温差引起的水密度的差异是热分层现象的主要原因。基于环境流体动力学代码(EFDC)模型,盐米德被用作陡峭地形的案例研究。 SIG坐标在顶部和中水层的校准温度时间序列之间产生密切一致,但底部水层的差距。由于SIG坐标变换,误差在水平压力梯度误差中出现。既不增加垂直分辨率也不是调整水平粘度系数的解析这个误差。我们测试Sigma-zed(sgz)坐标,将z坐标和sig坐标作为SIG坐标的替代,以找到它们有效地降低了模型的运行时间和仿真效率。 SGZ坐标模式下的垂直温度分布比SIG坐标模式的分布更准确。在SIG坐标下,Navier-Stokes水平梯度和平坦扩散方程导致对压力梯度非常敏感。替代品还增强了热控附近的分辨率,有助于重点水底部和相等的Sigma表面,在局部深水与陡峭地形的局部深水模拟方面具有显着的优势,并缩短运行时为0.14?h。建议使用SGZ混合坐标在模拟深水湖泊或储层中,其中水下地形大(具有丰富的连续深沟或珊瑚礁)。

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