首页> 外文会议>International Conference on Modeling, Simulation and Applied Optimization >Assessment of the hydrological response of the watershed through a distributed physically-based modeling for extreme events: Application in the Raghay catchment (Medjerda) (Northern Tunisia)
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Assessment of the hydrological response of the watershed through a distributed physically-based modeling for extreme events: Application in the Raghay catchment (Medjerda) (Northern Tunisia)

机译:评估流域的水性响应通过分布式的物理模型进行极端事件:在拉格艇集水区(Medjerda)(突尼斯北部)的应用

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This research study consists on the validation of the physically and distributed hydrological model, throw the application of the ATHYS platform for hydrological modeling, for the case study of a catchment area situated in the left bank of the high valley of the Medjerda basin, the catchment area of the Raghay wadi having an area of approximately 322 km. This watershed is characterized by a very important morphological, climatic and physical variability in time and space, often presenting very important floods because of the not measured flow coming from the Algerian frontier part instead of the large difference of atitude from 165 to 1180 in the Tunisian part. The choice is fixed on six events distributed over three different seasons, recorded on the level of two pluviographic stations for an hour time-step and which control the flow in the discharge system of the catchment area. The parameters of entry of the GREEN and AMPT production function are maps having the variability of the physical parameters of the soil as well as the variation of altitude and of the directions of drainage. The advantage of this function is related on its physical base, and the theoretical possibility to estimate and optimize the parameters starting from data of grounds or “in situ” measurements. The evaluated criteria for optimization are the Nash criteria which is varying between 0.73 and 0.98 for the calibration phase, and between 0.62 and 0.75 for the validation for the three seasons, instead of the Arithmetic Mean Error for the volume and the peak flow giving very good errors for the Wintry season, good errors for the Autumnal season and medium errors for the Springer season. The results of simulations show that the selected model is well validated for the Raghay catchment than, its performance in the comprehension of the hydrological answer of a Mediterranean watershed, which provide important information for decision makers in order of protection again- t floods of the area.
机译:该研究包括对物理和分布式水文模型的验证,抛出了Athys of Fathtology Modeling的应用程序,为位于Medjerda盆地的高山左岸的集水区的案例研究Raghay Wadi的面积约322公里。该流域的特点是在时间和空间中具有非常重要的形态,气候和物理变化,通常由于来自阿尔及利亚前部的未测量的流量而不是从突尼斯的165到1180的职业从165到1180的典型差异呈现非常重要的洪水部分。选择在三个不同季节的六个事件中修复,记录在两个Pluvographic站的水平上,一小时时间步长,并控制集水区的放电系统中的流量。绿色和AMPT生产功能的进入参数是具有土壤物理参数的可变性的地图以及海拔高度和排水方向的变化。此功能的优点在其物理基础上是相关的,以及估计和优化从地面数据或“原位”测量开始的参数的理论可能性。优化的评估标准是纳什标准,校准阶段的0.73和0.98之间变化,对于三个季节的验证,而不是0.62和0.75,而不是体积的算术平均误差,并且峰值流量非常好冬季季节的错误,秋季季节的良好错误和斯普林克季节的媒体错误。模拟结果表明,所选模型对于拉格滨集水区的验证良好,其表现在理解地中海流域的水文答案方面的性能,这为决策者提供了重要信息,以便在该地区的洪水泛滥。

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