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首页> 外文期刊>San Francisco Estuary and Watershed Science >Three-Dimensional Modeling of Hydrodynamics and Salinity in the San Francisco Estuary: An Evaluation of Model Accuracy, X2, and the Low–Salinity Zone
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Three-Dimensional Modeling of Hydrodynamics and Salinity in the San Francisco Estuary: An Evaluation of Model Accuracy, X2, and the Low–Salinity Zone

机译:旧金山河口水动力和盐度的三维建模:模型精度,X2和低盐度区的评估

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doi: http://dx.doi.org/10.15447/sfews.2015v13iss1art2 The three-dimensional UnTRIM San Francisco Bay–Delta model was applied to simulate tidal hydrodynamics and salinity in the San Francisco Estuary (estuary) using an unstructured grid. We compared model predictions to observations of water level, tidal flow, current speed, and salinity collected at 137 locations throughout the estuary. A quantitative approach based on multiple model assessment metrics was used to evaluate the model's accuracy for each comparison. These comparisons demonstrate that the model accurately predicted water level, tidal flow, and salinity during a 3-year simulation period that spanned a large range of flow and salinity conditions. The model is therefore suitable for detailed investigation of circulation patterns and salinity distributions in the estuary. The model was used to investigate the location, and spatial and temporal extent of the low-salinity zone (LSZ), defined by salinity between 0.5 and 6 psu. We calculated X2, the distance up the axis of the estuary to the daily-averaged 2-psu near-bed salinity, and the spatial extent of the LSZ for each day during the 3-year simulation. The location, area, volume, and average depth of the low-salinity zone varied with X2; however this variation was not monotonic and was largely controlled by the geometry of the estuary. We used predicted daily X2 values and the corresponding daily Delta outflow for each day during the 3-year simulation to develop a new equation to relate X2 to Delta outflow. This equation provides a conceptual improvement over previous equations by allowing the time constant for daily changes in X2 to vary with flow conditions. This improvement resulted in a smaller average error in X2 prediction than previous equations. These analyses demonstrate that a well-calibrated three-dimensional (3-D) hydrodynamic model is a valuable tool for investigating the salinity distributions in the estuary, and their influence on the distribution and abundance of physical habitat.
机译:doi:http://dx.doi.org/10.15447/sfews.2015v13iss1art2三维UnTRIM旧金山湾-三角洲模型被用于使用非结构化网格模拟旧金山河口(河口)中的潮汐水动力和盐度。我们将模型预测与观察到的整个河口137个位置的水位,潮汐流,当前速度和盐度进行了比较。基于多个模型评估指标的定量方法用于评估每个比较的模型准确性。这些比较表明,该模型可以在3年的模拟期内准确预测水位,潮汐流量和盐度,该模拟跨越了大范围的流量和盐度条件。因此,该模型适合详细研究河口的循环模式和盐分分布。该模型用于调查低盐度带(LSZ)的位置,时空范围,该范围由0.5至6 psu的盐度定义。我们计算了X2,河口轴到日平均2 psu近床盐度的距离,以及3年模拟期间每天的LSZ的空间范围。低盐度区的位置,面积,体积和平均深度随X2的变化而变化。然而,这种变化不是单调的,并且很大程度上受河口的几何形状控制。在3年的模拟期间,我们使用了每天的预测X2值和每天相应的每日Delta流出量,以开发一个新的公式将X2与Delta流出量相关联。该公式通过允许X2的每日变化的时间常数随流量条件而变化,从而对以前的公式进行了概念上的改进。这种改进导致X2预测中的平均误差比以前的方程式要小。这些分析表明,经过良好校准的三维(3-D)水动力模型是研究河口盐分分布及其对物理栖息地分布和丰富度的影响的宝贵工具。

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