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Evaluating flash flood simulation capability with respect to rainfall temporal variability in a small mountainous catchment

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Abstract

Rainfall temporal patterns significantly affect variability of flash flood behaviors, and further act on hydrological model performances in operational flash flood forecasting and warning. In this study, multivariate statistical analysis and hydrological simulations (XAJ and CNFF models) were combined to identify typical rainfall temporal patterns and evaluate model simulation capability for water balances, hydrographs, and flash flood behaviors under various rainfall patterns. Results showed that all the rainfall events were clustered into three types (Type 1, Type 2, and Type 3) in Anhe catchment in southeastern China. Type 1 was characterized by small total amount, high intensity, short duration, early peak moment, and concentrated hourly distribution. Type 3 was characterized by great total amount, low intensity, long duration, late peak moment, and uniform hourly distribution. Characteristics of Type 2 laid between those of Type 1 and Type 3. XAJ and CNFF better simulated water balances and hydrographs for Type 3, as well as all flash flood behavior indices and flood dynamics indices. Flood peak indices were competitively simulated for all the types by XAJ and except Type 1 by CNFF. The study is of significance for understanding relationships between rainfall and flash flood behaviors and accurately evaluating flash flood simulations.

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Correspondence to Xiaoyan Zhai.

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Foundation: National Natural Science Foundation of China, No.42171047, No.42071041

Author: Wang Xuemei (1998–), PhD Candidate, specialized in hydrology and water resources. E-mail: wang_xmww@163.com

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Evaluating flash flood simulation capability with respect to rainfall temporal variability in a small mountainous catchment

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Wang, X., Zhai, X., Zhang, Y. et al. Evaluating flash flood simulation capability with respect to rainfall temporal variability in a small mountainous catchment. J. Geogr. Sci. 33, 2530–2548 (2023). https://doi.org/10.1007/s11442-023-2188-5

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  • DOI: https://doi.org/10.1007/s11442-023-2188-5

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