首页> 外文会议>IAHR World Congress >THE ADJUSTMENT OF C-BAND RADAR-RAINFALL ESTIMATES AND ITS IMPACT ON STREAM FLOW SIMULATION UNCERTAINTY: A CASE STUDY FOR JAKARTA URBAN RIVER BASIN, INDONESIA
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THE ADJUSTMENT OF C-BAND RADAR-RAINFALL ESTIMATES AND ITS IMPACT ON STREAM FLOW SIMULATION UNCERTAINTY: A CASE STUDY FOR JAKARTA URBAN RIVER BASIN, INDONESIA

机译:C波段雷达降雨估计的调整及其对流流量模拟不确定性的影响 - 以印度尼西亚雅加达城市河流盆地为例

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The utilization of weather radar has shown the considerable potential for improving the distributed rainfall estimation and prediction of flood. Ciliwung River in Indonesia (476 km~2) has notably contributed to the recurrent flooding in Jakarta. C-band weather radar is available for providing rain information in Greater Jakarta. Yet, as single polarimetric radar, the verification of its observation with point rain gauge measurements is indispensable. In this study, the strategies of radar-rainfall calibration and adjustment for extracting radar estimates that is consistent with the ongoing development of real-time flood prediction in Ciliwung River is designed. Furthermore, the impact of the adjusted radar-rainfall estimates on the rainfall-runoff simulation is investigated. The radar reflectivity is converted to rainfall intensity by Z-R algorithms. Several storm events are selected to evaluate the appropriate Z-R relation by minimizing the mean square error between rain gauges and radar-rainfall in offline scheme. Applying the predefined Z-R relation, the remaining biases in the radar-rainfall estimates are corrected by using bias adjustment factor method calculated as the ratio between the accumulated rain gauge rainfall and accumulated radar-rainfall. The rainfall estimates without adjustment, by Marshall-Palmer Z-R algorithm, calibrated radar-rainfall, and adjusted radar-rainfall are introduced to physically distributed hydrological model in hourly basis. The simulated runoff is evaluated at Katulampa, Depok, and MT. Haryono points representing upstream, middle stream, and downstream outlets. Along with these three inputs, the uncertainties of hydrological model parameter are assessed. Through the calibration process, the algorithm with the lowest error for Ciliwung River basin is obtained. The analysis reveals that the different radar verification methods account for the variation in the performance of simulated flood. The results suggest the importance of correction of rainfall estimated from C-band non-polarimetric radar observation. The proposed framework on radar-rainfall utilization for real-time flood prediction system in Ciliwung River is also discussed.
机译:天气雷达的利用显示了改善分布式降雨估计和洪水预测的相当大。印度尼西亚的Ciliwung河(476公里〜2)显着促进了雅加达的经常性洪水。 C波段天气雷达可用于在大雅加达提供雨量信息。然而,作为单偏振雷达,用点雨量测量测量的观察结果是必不可少的。在这项研究中,设计了雷达降雨校准和调整,提取与Ciliwung River河实时洪水预测持续发展的雷达估计的调整。此外,研究了调整后的雷达降雨降雨估计对降雨径流模拟的影响。通过Z-R算法将雷达反射率转换为降雨强度。选择几种风暴事件以通过最小化雨量仪和离线方案的雷达降雨之间的均方误差来评估适当的Z-R关系。应用预定义的Z-R关系,通过使用偏置调节因子方法作为累积的雨量降低降雨与累积雷达降雨之间的比率计算的偏压调节因子方法来校正雷达降雨估计中的剩余偏差。没有调整的降雨估计,由Marshall-Palmer Z-R算法,校准雷达降雨和调整后的雷达降雨量在小时内以物理分布的水文模型引入。模拟的径流在Katulampa,Depok和Mt处进行评估。哈里诺积分代表上游,中游和下游出口。随着这三个输入,评估水文模型参数的不确定性。通过校准过程,获得了Ciliwung河流域最低误差的算法。该分析表明,不同的雷达验证方法占模拟洪水性能的变化。结果表明,从C波段非极化雷达观察估算降雨估算的重要性。还讨论了Ciliwung河实时洪水预测系统的雷达降雨利用框架。

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