首页> 外文会议>Proceedings of the Ninth International Symposium on River Sedimentation vol.4 >PROBABILISTIC EVALUATION OF FLOW DURATION CURVES IN SEMI-ARID BASINS
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PROBABILISTIC EVALUATION OF FLOW DURATION CURVES IN SEMI-ARID BASINS

机译:半干旱盆地中流动持续时间曲线的概率评估

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The flow duration curve (FDC) is a relationship between any given discharge value and the percentage of time that this discharge is exceeded, or, in other words, the relationship between magnitude and frequency of streamflow discharges. In this work, according to a probabilistic approach to the FDCs, the percentage of time is considered as a fraction of the year and the FDC is derived linking each discharge to the expected value of the fraction of the year during which such discharge is exceeded. In particular, a method for the evaluation of the FDC with a fixed return period T (T-year FDC) is proposed. The FDC is considered as a function bounded above and below. The upper and lower bounds are assumed equal to the corresponding T-year fractiles of, respectively, the annual maximum aftd minimum probability distribution of the mean daily discharge. The FDC is then modeled as a logarithmic transformed discharge following a Pearson Type 1 distribution (Beta function). In the case of intermittent flow regimes, which characterize the study cases presented (Puglia, Southern Italy), such approach had to be used in order to produce a satisfactory agreement between abserved and modeled FDCs. The methodology proposed seems promising in the framework of the regional evaluation of the T-year FDCs and when dealing with ungauged river catchments.
机译:流动持续时间曲线(FDC)是任何给定的排放值和超过该排放的时间百分比之间的关系,换句话说,是流量排放的大小和频率之间的关系。在这项工作中,根据对FDC的概率方法,将时间百分比视为一年的一小部分,并得出FDC,将每次排放与超过该排放的那部分年的期望值联系起来。特别地,提出了一种用于评估具有固定回报期T(T年FDC)的FDC的方法。 FDC被视为上方和下方的功能。假定上限和下限分别等于平均日排放量的年度最大后最小概率分布的相应T年分数。然后将FDC建模为遵循Pearson类型1分布(Beta函数)的对数转换放电。在以所介绍的研究案例为特征的间歇流动状态的情况下(意大利南部普利亚),必须使用这种方法才能在观测的和模拟的FDC之间达成令人满意的协议。所提出的方法论在T年FDCs的区域评估框架中以及在处理未开垦的河流集水区时似乎很有希望。

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