Flood Estimation Studies Using Hydrologic Modelling System (HEC-HMS) For Batu Pahat River Malaysia

Aiman Fahd Mahmood Mohammed, M. Adnan, Amgad Muneer, Safwan Sadeq
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Abstract

Discharge is an important parameter that required in predicting flood events, especially those with great magnitudes. The outcomes of these predictions form an important part of the understanding and control risks of flooding knowledge for the authorities, planners and the general public. The hydrological data could be used to analyze the river system's reaction to deep rainfall and to draw up flood hydrographs with fair precision using the required rainfall-runoff model from the details of the rainfall. The aim of this study to understand the rainfall and water level trend for the last 11 years which was used to estimate the flow discharge derived from rainfall data for Batu Pahat, Johor. The data of rainfall and water level was collected from DID Malaysia for two different stations in Batu Pahat, which represent the rainfall and water level data for the last 10 years. Mann Kendall method was utilized to analyses the trend of these hydrological data. While the HEC-HMS software was used to estimate the flow discharge data that applied the suitable analyses method. Mann Kendall test shows the Kendall's tau value was −0.233 and −0.437 for rainfall and water level respectively. The indicated a decreasing trend for both parameters but the trend is no significant. This might be due to the missing data within these 10 years. By referring to the discharge result, it shows that the value of runoff is increase with the increasing of rainfall where the maximum value of discharge is about 960.6 cfs. Thus, based on this value, it could give an insight to the local authority to plan their strategy to accommodate this discharge within the river reach to minimize the flood event.
利用水文模拟系统(HEC-HMS)对马来西亚巴哈河进行洪水估算研究
流量是预测洪水灾害,特别是特大洪水灾害的重要参数。这些预测的结果构成了当局、规划者和公众了解和控制洪水风险知识的重要组成部分。水文数据可以用来分析河流系统对强降雨的反应,并根据降雨的细节使用所需的降雨-径流模型,以相当精确的方式绘制洪水曲线。本研究的目的是了解近11年的降雨量和水位趋势,并利用降雨资料估算柔佛州巴都巴合的流量。降雨和水位数据来自马来西亚气象署在巴都巴哈特的两个不同站点,它们代表了过去10年的降雨和水位数据。利用Mann - Kendall方法对水文资料的变化趋势进行了分析。采用HEC-HMS软件对采用合适分析方法的流量数据进行估算。Mann Kendall检验表明,降雨量和水位的Kendall tau值分别为- 0.233和- 0.437。结果表明,两个参数均有减小的趋势,但减小的趋势不显著。这可能是由于这10年的数据缺失所致。从径流量结果可以看出,径流量随降雨量的增加而增加,径流量最大值约为960.6 cfs。因此,基于这个值,它可以为地方当局提供洞察,以规划他们的策略,以适应河流范围内的这种排放,以尽量减少洪水事件。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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