首页> 外文会议>Asian conference on remote sensing;ACRS >CALIBRATION OF WATERSHED LAG TIME EQUATION FOR PHILIPPINE HYDROLOGY USING RADARSAT DIGITAL ELEVATION MODEL
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CALIBRATION OF WATERSHED LAG TIME EQUATION FOR PHILIPPINE HYDROLOGY USING RADARSAT DIGITAL ELEVATION MODEL

机译:基于雷达数字高程模型的菲律宾水文流域滞后时间方程式的标定

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Widespread flooding is a major problem in the Philippines. The country experiences heavy amount of rainfall throughout the year and several areas are prone to flood hazards because of its unique topography. Human casualties and destruction of infrastructure are some of the damages caused by flooding and the Philippine government has undertaken various efforts to mitigate these hazards. One of the solutions was to create flood hazard maps of different floodplains and use them to predict the possible catastrophic results of different rain scenarios. To produce these maps with accurate output, different input parameters were needed and one of those is calculating hydrological components from topographical data. This paper presents how a calibrated lag time equation was obtained using measurable catchment parameters. Lag time is an essential input in flood mapping and is defined as the duration between the peak rainfall and peak discharge of the watershed. The lag time equation involves measurable parameters, namely, watershed length and watershed slope, which were both available from RADARSAT Digital Elevation Models (DEM). The equation also involves the maximum potential retention of the soil derived from its curve number which was processed from the Philippine Curve Number Map. This approach was based on a similar method developed by CH2M Hill and Horritt for Taiwan, which has a similar set of meteorological and hydrological parameters with the Philippines. Rainfall data from fourteen water level sensors covering 67 storms from all the regions in the country were used to measure actual lag time values. The measured lag time values were plotted against the calculated values obtained from the Natural Resource Conservation Management handbook lag time equation. Regression analysis was used to obtain the final calibrated equation that would be used to calculate the lag time specifically for rivers in the Philippines. The calculated lag time values could then be used as a parameter for modeling different flood scenarios in the country.
机译:泛滥是菲律宾的一个主要问题。该国全年降雨量很大,并且由于其独特的地形,一些地区容易遭受洪灾危害。洪水造成的人员伤亡和基础设施的破坏是其中的一部分,菲律宾政府已采取各种措施来减轻这些危害。解决方案之一是创建不同洪泛区的洪水灾害图,并使用它们来预测不同降雨情景的可能灾难性后果。为了生成具有精确输出的这些地图,需要使用不同的输入参数,其中之一是根据地形数据计算水文分量。本文介绍了如何使用可测量的流域参数获得校准的滞后时间方程。滞后时间是洪水地图绘制中必不可少的输入,并且定义为高峰降雨与流域洪峰排放之间的持续时间。滞后时间方程涉及可测量参数,即分水岭长度和分水岭坡度,这两个参数均可从RADARSAT数字高程模型(DEM)获得。该方程还涉及从土壤曲线数得出的土壤最大潜在保留力,该曲线数是根据菲律宾曲线数图处理的。这种方法基于CH2M Hill和Horritt为台湾开发的类似方法,该方法与菲律宾具有相似的气象和水文参数集。来自十四个水位传感器的雨量数据覆盖了该国所有地区的67次暴风雨,用于测量实际滞后时间值。将测得的滞后时间值与从《自然资源保护管理手册》滞后时间方程式中获得的计算值作图。回归分析用于获得最终的校准方程,该方程将用于计算专门针对菲律宾河流的滞后时间。然后可以将计算出的滞后时间值用作模拟该国不同洪水情景的参数。

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