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在水文样本服从统一分布的前提下,水文频率分析才可以有效地进行计算。同时,水文样本无论是过去还是现在,或是在将来,都必须具有强烈的同步性和一致性,才能满足水文频率分析的随机同步假设的要求。此时,非一致性水文频率分析的方法就显得尤为重要。本文就非一致性水文频率分析的方法做出了研究,以期为水文频率分析的研究带来一定程度上的帮助。
Hydrological frequency analysis can be effectively calculated under the assumption of uniform distribution of hydrological samples. At the same time, hydrological samples, whether past, present or future, must be strongly synchronized and consistent in order to meet the requirements of stochastic synchronization assumptions for hydrological frequency analysis. At this point, the method of non-uniform hydrological frequency analysis is particularly important. In this paper, we study on the method of non-uniform hydrological frequency analysis, with a view to a certain degree of help for the study of hydrological frequency analysis.