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TOWARDS A 3D HYDRODYNAMIC NUMERICAL MODELING SYSTEM FOR LONG TERM SIMULATIONS OF THE RIO DE LA PLATA DYNAMIC

机译:朝着Rio de la Plata的长期模拟3D流体动力学数值模拟系统

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In order to support water management decisions involving characteristics of the Rio de la Plata current fields, a 3D hydrodynamic baroclinic numerical model has been implemented. Firstly, a 2D South Atlantic hydrodynamic barotropic model forced by NCEP reanalysis winds and the astronomical model FES2004, called 'AStide' is implemented and calibrated, taking the quality in the representation of the water level oscillations at the mouth of the Rio de la Plata as the calibration condition. Secondly, a 3D hydrodynamic baroclinic model, with ten vertical sigma layers, forced for fluvial discharges, ECWMF reanalysis winds and boundary conditions from the AStide model, called 'RPtide' is implemented and calibrated. The computational tool used for the simulations is based on the MOHID water system and was developed with the aim of achieving a good quality in the dynamic representation while maintaining independence in the execution and efficient computation times. In order to improve the performance of the tool, several HPC techniques were applied, achieving speedups of up to 2×, while further improvements on the computational schemes used in the model allowed a 25% reduction in the running time. The proposed tool was used and validated, based on a hindcast strategy using the MOHID water system, in the evaluation of the potential energy of tidal currents in the area.
机译:为了支持涉及Rio de La Plata电流场特性的水管理决策,已经实施了3D流体动力学曲金数值模型。首先,通过NCEP Reanalysis Winds强迫的2D南大西洋流体动力学波调模型和称为“静脉”的天文模型FES2004,并校准了Rio de La Plata口处的水位振荡的质量校准条件。其次,利用十个垂直Σ层的3D流体动力学羧基模型被迫从河流放电,ECWMF再分析风和来自静物模型的边界条件,称为“RPTIDE”,并校准。用于仿真的计算工具基于Mohid水系统,并且目的是在动态表示中实现良好质量的目的,同时在执行和有效的计算时间内保持独立性。为了提高该工具的性能,应用了几种HPC技术,实现了高达2倍的加速度,而模型中使用的计算方案的进一步改进允许运行时间减少25%。基于使用Mohid水系统的Hindcast策略,在评估该地区的潮流势能的评估中,使用并验证了该工具并验证。

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