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KNN-based local linear regression for the analysis and simulation of low flow extremes under climatic influence

机译:基于KNN的局部线性回归用于气候影响下低流量极端的分析和模拟

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Climate change frequently causes highly nonlinear and irregular behaviors in hydroclimatic systems. The stochastic simulation of hydroclimatic variables reproduces such irregular behaviors and is beneficial for assessing their impact on other regimes. The objective of the current study is to propose a novel method, a k-nearest neighbor (KNN) based on the local linear regression method (KLR), to reproduce nonlinear and heteroscedastic relations in hydroclimatic variables. The proposed model was validated with a nonlinear, heteroscedastic, lag-1 time dependent test function. The validation results of the test function show that the key statistics, nonlinear dependence, and heteroscedascity of the test data are reproduced well by the KLR model. In contrast, a traditional resampling technique, KNN resampling (KNNR), shows some biases with respect to key statistics, such as the variance and lag-1 correlation. Furthermore, the proposed KLR model was used to simulate the annual minimum of the consecutive 7-day average daily mean flow (Min7D) of the Romaine River, Quebec. The observed and extended North Atlantic Oscillation (NAO) index is incorporated into the model. The case study results of the observed period illustrate that the KLR model sufficiently reproduced key statistics and the nonlinear heteroscedasticity relation. For the future period, a lower mean is observed, which indicates that drier conditions other than normal might be expected in the next decade in the Romaine River. Overall, it is concluded that the KLR model can be a good alternative for simulating irregular and nonlinear behaviors in hydroclimatic variables.
机译:气候变化经常导致水文气候系统高度非线性和不规则行为。水文气候变量的随机模拟重现了这种不规则行为,有利于评估它们对其他制度的影响。本研究的目的是提出一种新方法,即基于局部线性回归方法(KLR)的k最近邻(KNN),以再现水文气候变量中的非线性和异方差关系。所提出的模型已通过非线性,异方差,滞后1时间相关的测试函数进行了验证。测试函数的验证结果表明,KLR模型可以很好地再现测试数据的关键统计量,非线性相关性和异方差性。相反,传统的重采样技术,即KNN重采样(KNNR),相对于关键统计数据显示出一些偏差,例如方差和lag-1相关性。此外,提出的KLR模型用于模拟魁北克罗曼河的连续7天平均每日平均流量(Min7D)的年最小值。观测到的北大西洋涛动指数和扩展后的北大西洋涛动指数均纳入模型。观察期的案例研究结果表明,KLR模型充分再现了关键统计数据和非线性异方差关系。对于未来时期,观测到的平均值较低,这表明在未来十年内,长叶河流域可能会出现比正常情况更干燥的状况。总的来说,可以得出结论,KLR模型可以很好地替代模拟水文气候变量中的不规则和非线性行为。

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