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HYDRODYNAMIC CHARACTERIZATION OF BAIA DE TODOS OS SANTOS-BA USING NUMERICAL MODELING

机译:使用数值模拟的Baia de Todos OS Santos-Ba的流体动力学表征

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Baia de Todos os Santos (BTS) is the second largest bay at Brazilian coast, being surrounded by 12 cities, among those Salvador, the capital of the state of Bahia. BTS presents environmental problems caused by disorderly occupation and an accelerated industrialization process. To better understand the BTS's circulation, a 2DH hydrodynamic model was generated using DELFT3D. Bathymetry and wind time series used as input to the model in this project as well as the measured data in situ (water level and depth average velocity) were collected by the program Bahia Azul and shared by professor Paulo C. C. Rosman (COPPE/UFRJ). Sea boundaries used astronomic constituents calculated for Salvador's Harbour were used. The model was validated through statistical methods R~2 and Mean Absolute Error (MAE) for water level, depth average velocity and total energy spectrum. Results showed that BTS has small influence of sub-inertial frequencies and river discharge, being mainly influenced by astronomical tide. Higher values of depth average velocity were found at BTS's outlet. At neap tide high peak velocity for depth average velocity is 1.0 m/s for both inflow and outflow and at spring tide depth average velocity reaches 1.6 m/s and 1.9 m/s for outflow and inflow, respectively. Inside the bay the water level varies between -0.5 m and 0.65 m at neap tide and -1.5 m and 1.5 m at spring tide. In total, 9 observation points were compared with measured data. Better results were found inside the bay with R~2 as high as 0.8994, 0.8411, 0.9236 and 0.9996 for water level, U and V depth average velocity component and total energy spectrum, respectively. Observation points in open sea, close to boundaries presented worst results, mostly in U and V depth average velocity components, showing results as low as 0.0060 and 0.0541, respectively. This can be explained by the proximity of the boundary and also because the presence of a sub-inertial frequency, not calculated in this model. The numerical results showed that the model could accurately predict the flow dynamics inside de BTS bay.
机译:Baia de Todos Os Santos(BTS)是巴西海岸的第二大湾,被12个城市包围,其中萨尔瓦多,巴伊亚州的首都。 BTS呈现因占用和加速工业化过程引起的环境问题。为了更好地理解BTS的循环,使用Delft3D产生2DH流体动力学模型。由Paira Azul的计划收集了作为该项目的模型的浴室和风时间序列以及原位(水位和深度平均速度)的测量数据,并由Paulo C. Rosman(Coppe / UFRJ)分享。使用海边使用对萨尔瓦多港口计算的天文学成分。该模型通过统计方法R〜2和平均绝对误差(MAE)进行验证,深度平均速度和总能量谱。结果表明,BTS对亚惯性频率和河流放电的影响小,主要受天文潮的影响。 BTS的出口发现了更高的深度平均速度值。在NeAP潮中,对于流入和流出,流入和流出的高峰速度为1.0 m / s,春季潮汐平均速度分别达到1.6米/秒和1.9米/秒,用于流出和流入。海湾内部水位在NeAP潮汐下的-0.5米和0.65米之间变化,春报的速度为-1.5 m和1.5米。总共与测量数据进行比较9个观察点。在海湾内部发现了更好的结果,R〜2高达0.8994,0.8411,0.9236和0.9996,用于水位,U和V深度平均速度分量和总能谱。近海的观察点,接近边界呈现最差的结果,主要是在U和V深度平均速度分量中,显示出低至0.0060和0.0541的结果。这可以通过边界的接近来解释,并且还因为在该模型中不计算的子惯性频率的存在。数值结果表明,该模型可以准确地预测DE BTS湾内的流动动态。

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