Modeling run-off flow hydrographs using remote sensing data: an application to the Bashar basin, Iran

M. Rafiee, Sattar Rad, Mehdi Mahbod, Masih Zolghadr, Ravi Prakash Tripathi, H. M. Azamatulla
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Abstract

Precipitation, as one of the most significant parameters in hydrological simulations, is often difficult accessible in countries, such as Iran, due to an inadequate number of rain gauge stations. Remote sensing has provided an alternative source using a specific spatial and temporal resolution in rainfall estimation throughout an area. In this study, the effectiveness of the Hydrologic Engineering Center-Hydrologic Modeling System runoff rainfall simulation model was evaluated using the Global Precipitation Measurement (GPM) Mission satellite and rain gauge station precipitation data. The model was calibrated and validated using five flood event data of a hydrometric station at the outlet of the Bashar basin. Most important flood parameters including peak discharge (QP), flood volume (V) and time of concentration (TC) were used to evaluate and compare the application of satellite and ground station data in the model using various statistical indices. The accuracy of QP and V estimations by using rain gauge data was higher than those obtained by satellite data. However, the difference between mean relative error (MRE) in QP estimation was less than 1% (9.9 and 10.6% for rain gauge and satellite data, respectively). Conversely, higher accuracies were met for TC estimation using satellite (with MRE 9.1 and 10.2% for GPM and rain gauge data, respectively).
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利用遥感数据建立径流量水文图模型:在伊朗巴沙尔盆地的应用
降雨量是水文模拟中最重要的参数之一,但在伊朗等国家,由于雨量站数量不足,通常很难获得降雨量。遥感技术利用特定的空间和时间分辨率为估算整个地区的降雨量提供了一种替代来源。在这项研究中,利用全球降水测量(GPM)任务卫星和雨量站降水数据,对水文工程中心-水文建模系统径流降雨模拟模型的有效性进行了评估。利用巴沙尔流域出口水文站的五次洪水事件数据对模型进行了校准和验证。最重要的洪水参数包括洪峰流量 (QP)、洪水流量 (V) 和集中时间 (TC),利用各种统计指数对模型中卫星和地面站数据的应用进行了评估和比较。利用雨量计数据估算的 QP 和 V 的准确度高于卫星数据。然而,QP 估算的平均相对误差(MRE)相差不到 1%(雨量计和卫星数据分别为 9.9% 和 10.6%)。相反,利用卫星数据估算 TC 的精度更高(GPM 和雨量计数据的平均相对误差分别为 9.1% 和 10.2%)。
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