为建立分析模型而进行的深度过程数据挖掘: 2. 冬春气温和降水对山区河流春季极端洪水的影响

Yuri Kirsta, I. Troshkova
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引用次数: 0

摘要

使用称为系统分析建模的深度过程数据挖掘的标准方法,我们建立了一个高性能的过程驱动(分析)模型,用于描述冬春温度和降水对山区河流春季极端洪水的影响。4月,洪峰(伴有冰的移动)造成紧急洪水泛滥,对当地居民构成持续的威胁。以阿尔泰-萨延山区34条中小河流为例,分析了1951-2020年4月流域景观结构、冬春气温和降水对春季洪峰谷流量(SFDP和SFDT)的影响。我们确定了SFDP/SFDT对气象条件的非平凡依赖,提出了它们的物理水文实质,并确定了SFDP/SFDT对气象因子变化的敏感性作为观测到的SFDP/SFDT方差的贡献。冬季和春季降水、冬季气温和春季气温对SFDP/SFDT方差的贡献分别为34.7%、21.9%、7.8、6.1%和13.6%、18.8%、6.6、1.5%。
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DEEP PROCESS-DATA MINING FOR BUILDING OF ANALYTICAL MODELS: 2. INFLUENCE OF WINTER-SPRING TEMPERATURES AND PRECIPITATION ON SPRING FLOOD EXTREMES FOR MOUNTAIN RIVERS
Using the standard methodology for deep process-data mining called system- analytical modeling, we have built a high-performance process-driven (analytical) model for description of winter-spring temperatures and precipitation influence on spring flood extremes for mountain rivers. In April, flood discharge peaks (with ice motion) cause emergency inun- dations and pose a constant threat to local population. The effect of the landscape structure of river basins, winter-spring temperatures and precipitation on spring flood discharge peaks and troughs (SFDP and SFDT) for April 1951–2020 was analyzed by the example of 34 medium and small rivers of the Altai-Sayan mountain country. We identified nontrivial SFDP/SFDT dependences on meteorological conditions, proposed their physical-hydrological substantia- tions and determined SFDP/SFDT sensitivities to meteorological factor variations as con- tributions to the observed SFDP/SFDT variances. The contributions of winter and spring precipitation, winter air temperatures and spring ones for SFDP/SFDT variances made up 34.7, 21.9, 7.8, 6.1% and 13.6, 18.8, 6.6, 1.5%, respectively.
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