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Fitting Depth-discharge Relationships In Rivers With Floodplains

机译:用洪泛区拟合河流的水深关系

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A statistical method based on a simple uniform flow depth-discharge model for a two-stage main channel-floodplain river section has been developed and tested for data from four hydrometric gauging stations. The depth-discharge rating curve fitting procedure is formulated as a piecewise regression problem. A simulated annealing algorithm is used to obtain the least-squares rating curve parameters, including the main channel-floodplain change-point, uncertainty of all parameter and discharge estimates is approximated by bootstrap techniques. The application of the methodology to field data showed an accurate agreement between the measured and the estimated depth-discharge relationships. A good agreement between the observed and estimated main channel-floodplain change-points was also achieved. Some difficulties, caused by factors such as unequal measurement error variance, infinite parameter estimates and the presence of more than two depth-discharge change points, were apparent; these are discussed.
机译:已经开发了一种基于简单均匀流量深度-流量模型的两阶段主河道-洪泛河段的统计方法,并针对来自四个水文计量站的数据进行了测试。深度-流量等级曲线拟合程序被表述为分段回归问题。使用模拟退火算法来获得最小二乘评级曲线参数,包括主通道-洪泛区变化点,所有参数的不确定性和排放估计值均通过自举技术进行近似。该方法在现场数据中的应用表明,测得的深度与流量之间的估计关系是准确的。在观察到的和估计的主要河道-洪泛区变化点之间也达成了良好的协议。显而易见的困难是由诸如不相等的测量误差方差,无限的参数估计以及存在两个以上的深度放电变化点等因素引起的;讨论这些。

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