Influence of output size of stochastic weather generators on common climate and hydrological statistical indices

被引:2
作者
Alodah, Abdullah [1 ,2 ]
Seidou, Ousmane [2 ,3 ]
机构
[1] Qassim Univ, Coll Engn, Dept Civil Engn, Buraydah Al Qassim 51431, Saudi Arabia
[2] Univ Ottawa, Fac Engn, Dept Civil Engn, 161 Louis Pasteur, Ottawa, ON K1N 6N5, Canada
[3] United Nations Univ, Inst Water Environm & Hlth, 204-175 Longwood Rd S, Hamilton, ON L8P 0A1, Canada
关键词
Stochastic weather generators; Stochastic hydrological modeling; Hydrometeorology; Hydrological risk assessment; Climate ensemble; Climate sensitivity; Climate realizations; Hydrological realizations; LOW-FREQUENCY VARIABILITY; MARKOV-CHAIN MODEL; DAILY PRECIPITATION; WATER-RESOURCES; LOESS PLATEAU; LARS-WG; CLIGEN; IMPACT; TEMPERATURE; SIMULATION;
D O I
10.1007/s00477-020-01825-w
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
While Stochastic Weather Generators (SWGs) are used intensively in climate and hydrological applications to simulate hydroclimatic time series and estimate risks and performance measures linked to climate variability, there have been few investigations into how many realizations are required for a robust estimation of these measures. Given the computational cost and time necessary to force climate-sensitive systems with multiple realizations, the estimation of the optimal number of synthetic time series to generate with a particular SWG for a predefined accuracy when estimating a particular risk or performance measure is particularly important. In this paper, the required number of realizations of five SWGs coupled with a SWAT model (the Soil and Water Assessment Tool) needed in order to achieve a predefined Relative Root Mean Square Error is investigated. The statistical indices used are the mean, standard deviation, skewness, and kurtosis of four hydroclimatic variables: precipitation, maximum and minimum temperature, and annual streamflow obtained for each observed and model-generated time series. While the results vary somewhat across SWGs, variables and indicators, they overall show that the marginal improvement decreases dramatically after 25 realizations. The results also indicate that the benefit of generating more than 100 realizations of climate and streamflow data is very minimal. The methodology presented herein can be applied in further investigations of other set of risk indicators, SWGs, hydrological models, and watersheds to minimize the required workload.
引用
收藏
页码:993 / 1021
页数:29
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