Uncertainty analysis and prediction of river runoff with multi-time scales

被引:11
|
作者
Zhang, Jinping [1 ]
Zhao, Yong [2 ]
Lin, Xiaomin [1 ]
机构
[1] Zhengzhou Univ, Sch Water Conservancy & Environm Engn, Zhengzhou 450001, Peoples R China
[2] China Inst Water Resources & Hydropower Res, State Key Lab Simulat & Regulat Water Cycle River, 1 Yuyuantan South Rd, Beijing 100038, Peoples R China
来源
关键词
cointegration theory; empirical mode decomposition; error correction model; runoff prediction; uncertainty; TIME-SERIES; NEURAL-NETWORKS;
D O I
10.2166/ws.2016.190
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Increasing water-issues demand that water resources managers know and predict the uncertain characteristics of river runoff well. In this paper, the fluctuating periods and local features of runoff with multi-time scales are analyzed by the empirical mode decomposition method. With the set pair analysis method, the uncertainty properties of runoff series with different multi-time scales are expressed. Meanwhile, cointegration theory is introduced to indicate the long-term equilibrium relationships between runoff series, and then the runoff prediction model is proposed based on the error correction model (ECM). The results show that the runoff series of Heihe River in northwest China exhibit complex relations with different periodic fluctuations and changing laws. The identity degree is the main relation between two runoff series, especially in the short period. Both the original series and decomposed components are all cointegrated, and the established runoff prediction model based on the ECM can simulate and predict river runoff well.
引用
收藏
页码:897 / 906
页数:10
相关论文
共 50 条
  • [1] Analysis of variation characteristics of runoff at multi-time scales under the influence of reservoir
    Yan, B.
    Zhang, X.
    Chen, Y. B.
    Yao, L. Q.
    Huang, F.
    Chen, Q. H.
    Gao, Q. S.
    Zhang, L. G.
    Guo, L. D.
    [J]. 5TH INTERNATIONAL CONFERENCE ON WATER RESOURCE AND ENVIRONMENT (WRE 2019), 2019, 344
  • [2] Component-based Reconstruction Prediction of Runoff at Multi-time Scales in the Source Area of the Yellow River Based on the ARMA Model
    Zhang, Jinping
    Xiao, Honglin
    Fang, Hongyuan
    [J]. WATER RESOURCES MANAGEMENT, 2022, 36 (01) : 433 - 448
  • [3] Component-based Reconstruction Prediction of Runoff at Multi-time Scales in the Source Area of the Yellow River Based on the ARMA Model
    Jinping Zhang
    Honglin Xiao
    Hongyuan Fang
    [J]. Water Resources Management, 2022, 36 : 433 - 448
  • [4] Study on the periodic fluctuations of runoff with multi-time scales based on set pair analysis
    Ye, Yan
    Zhang, Jinping
    Yang, Jiachun
    Li, Jian
    [J]. DESALINATION AND WATER TREATMENT, 2018, 129 : 332 - 336
  • [5] The joint probability distribution of runoff and sediment and its change characteristics with multi-time scales
    Zhang, Jinping
    Ding, Zhihong
    You, Jinjun
    [J]. JOURNAL OF HYDROLOGY AND HYDROMECHANICS, 2014, 62 (03) : 218 - 225
  • [6] Forecasting Analysis Based on Multi-scale and Multi-time with Uncertainty
    Park, Keon-Jun
    Son, Sung-Yong
    [J]. IFAC PAPERSONLINE, 2019, 52 (04): : 318 - 323
  • [7] Impact of reservoir operation on runoff and sediment load at multi-time scales based on entropy theory
    Zhang, Jinping
    Xiao, Honglin
    Zhang, Xin
    Li, Fawen
    [J]. JOURNAL OF HYDROLOGY, 2019, 569 : 809 - 815
  • [8] Determination of variation uncertainty in runoff time series at multi-temporal scales
    Ye, Yan
    Zhang, Jinping
    Long, Xunjian
    Ma, Lihua
    Ye, Yong
    [J]. JOURNAL OF WATER AND CLIMATE CHANGE, 2021, 12 (05) : 2010 - 2025
  • [9] Modeling and analysis of battery energy storage systems in multi-time scales application
    [J]. Lu, Q. (Luqiuyu22@126.com), 1600, Chinese Society for Electrical Engineering (33):
  • [10] Multi-time scale co-integration forecast of annual runoff in the source area of the Yellow River
    Zhang, Jinping
    Li, Hongbin
    Su, Bin
    Fang, Hongyuan
    [J]. JOURNAL OF WATER AND CLIMATE CHANGE, 2021, 12 (01) : 101 - 115