2014
DOI: 10.1007/s00477-014-0986-0
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A two-stage method of quantitative flood risk analysis for reservoir real-time operation using ensemble-based hydrologic forecasts

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Cited by 48 publications
(10 citation statements)
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“…Hydrological forecasting, especially medium and long-term runoff forecasting, is an indispensable part of water resources management and water conservancy projects' operation [1][2][3]. Forecasting at different time scales can provide valuable information for flood control, power generation, water supply, and drought resistance [4][5][6][7].…”
Section: Introductionmentioning
confidence: 99%
“…Hydrological forecasting, especially medium and long-term runoff forecasting, is an indispensable part of water resources management and water conservancy projects' operation [1][2][3]. Forecasting at different time scales can provide valuable information for flood control, power generation, water supply, and drought resistance [4][5][6][7].…”
Section: Introductionmentioning
confidence: 99%
“…Long-term hydrological prediction is of significance for water resource activities, such as reservoir operation [1][2][3][4][5], water resource planning [6][7][8][9], risk management [10][11][12][13], and urbanization [14,15]. Hence, hydrologic time-series forecasting, especially monthly inflow, has triggered great interest in hydrology and water resources fields [16,17].…”
Section: Introductionmentioning
confidence: 99%
“…The two‐stage theory developed by Liu, Lin, and Wei () is extended to the aggregation system. The two‐stage flood risk analysis equation for aggregation reservoirs is as follows: -6emRk()P=P()Send,kR()Send,k,PitalicdS=q=1FP()Send,k,qR()Send,k,q,P where, R k ( P ) is the flood risk with a flood of frequency P in the k th aggregation reservoir, F is the number of flood events, S end , k , q is the storage at the end of the pre‐discharge period of the k th aggregation reservoir with the q th flood, P ( S end, k , q ) is the storage probability at the end of the pre‐discharge operation for the k th aggregation reservoir with the q th flood, and R ( S end, k , q , P ) is the relationship between the storage and the flood risk of the k th aggregation reservoir with the q th flood.…”
Section: Methodsmentioning
confidence: 99%
“…For the multi‐reservoir operation, Tan et al () proposed a model that considered the capacity compensation of two reservoirs and the spatial uncertainty of flood characterisation using a confidence level that was subjective. Liu, Guo, Li, Chen, and Li (); Liu, Lin, and Wei () developed a two‐stage risk analysis method that used a forecast horizon point to divide future times into two stages (hydrological forecast lead time and unpredicted time), and effectively calculated the flood risk for single reservoirs. However, the risk analysis was affected by the issue of dimensionality as the number of reservoirs in the multi‐reservoir system increased.…”
Section: Introductionmentioning
confidence: 99%