Effect of heteroscedasticity treatment in residual error models on model calibration and prediction uncertainty estimation

被引:22
|
作者
Sun, Ruochen [1 ,2 ]
Yuan, Huiling [1 ,2 ,3 ]
Liu, Xiaoli [4 ]
机构
[1] Nanjing Univ, Sch Atmospher Sci, Nanjing 210023, Jiangsu, Peoples R China
[2] Nanjing Univ, Key Lab Mesoscale Severe Weather, Minist Educ, Nanjing 210023, Jiangsu, Peoples R China
[3] Joint Ctr Atmospher Radar Res CMA NJU, Nanjing, Jiangsu, Peoples R China
[4] Anhui Agr Univ, Sch Engn, Hefei, Anhui, Peoples R China
基金
中国国家自然科学基金;
关键词
Heteroscedasticity; Box-Cox transformation; Linear modeling method; Nonlinear modeling method; Residual error model; MONTE-CARLO-SIMULATION; PARAMETER-ESTIMATION; LIKELIHOOD FUNCTIONS; INFERENCE; AUTOCORRELATION; REPRESENTATION; PRECIPITATION; STREAMFLOW; JOINT;
D O I
10.1016/j.jhydrol.2017.09.041
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The heteroscedasticity treatment in residual error models directly impacts the model calibration and prediction uncertainty estimation. This study compares three methods to deal with the heteroscedasticity, including the explicit linear modeling (LM) method and nonlinear modeling (NL) method using hyperbolic tangent function, as well as the implicit Box-Cox transformation (BC). Then a combined approach (CA) combining the advantages of both LM and BC methods has been proposed. In conjunction with the first order autoregressive model and the skew exponential power (SEP) distribution, four residual error models are generated, namely LM-SEP, NL-SEP, BC-SEP and CA-SEP, and their corresponding likelihood functions are applied to the Variable Infiltration Capacity (VIC) hydrologic model over the Huaihe River basin, China. Results show that the LM-SEP yields the poorest streamflow predictions with the widest uncertainty band and unrealistic negative flows. The NL and BC methods can better deal with the heteroscedasticity and hence their corresponding predictive performances are improved, yet the negative flows cannot be avoided. The CA-SEP produces the most accurate predictions with the highest reliability and effectively avoids the negative flows, because the CA approach is capable of addressing the complicated heteroscedasticity over the study basin. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:680 / 692
页数:13
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