密云水库上游潮白河流域丰平枯特征及其与入库水量的定量关系
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1.水利部水土保持监测中心;2.北京林业大学

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S715

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Quantitative relationship between flood, normal and dry characteristics and inflow of Chaobai River basin in the upper reaches of Miyun Reservoir
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    摘要:

    [目的]揭示密云水库上游潮白河流域水量变化的年际时序规律及丰平枯季节性差异,为京津冀地区水资源高效利用及生态用水保障提供决策参考。[方法]在收集流域水量数据,进行潮白河流域逐月丰平枯水期分析的基础上,采用距平百分率解析潮白河流域水量变化特征,并推导流域丰平枯时段与径流水量的定量化关系。[结果]近12年来潮白河流域的枯水期历时远大于丰水期和平水期时间,但丰水水量及其距平百分比每隔1-2年均会呈现指数级增长趋势,表明潮白河流域近年来更多的表现出了极端的气候特征。潮白河流域的丰水时段均主要出现在7-12月,流域平水时段基本伴生于丰水时段,但12年来,潮河与白河流域分别仅出现了6、7个月的平水期;枯水时段占据了12年来的大部分时期,阶段性密集分布在除丰水期和平水期以外的所有时段。在所有时段,白河流域的水量均高于潮河流域,这可能归因于春季融雪对径流的补给。基于流量与丰枯时段的精细划分,构建了潮白河流域丰平枯水期与水量的定量化关系,其中流域丰平枯水期时段的占比大小是流域水量最重要的影响因素。[结论] 潮白河流域近年来极端降水时间增多,但枯水时段的占比远高于平水期和丰水期。三者的占比关系是影响流域水量最重要的因素。

    Abstract:

    [Objective] The inter-annual time-series pattern of water quantity change and the seasonal difference of abundance, flatness and dryness in the Chaobai River Basin upstream of the Miyun Reservoir were studied to provide decision support for efficient water utilization and ecological water security in the Beijing-Tianjin-Hebei region. [Methods] Based on the collection of water quantity data and the analysis of the monthly wet water period, normal water period and low water period, the distance flatness percentage was used to explore the characteristics of water quantity changes in the Chaobai River basin, and to derive the quantitative relationship between the abundance, flatness and dry periods of the basin and the amount of runoff water. [Results] In the past 12 years, the dry season time of the Chaobai River basin is much longer than the wet season and the flat season time, but the high-water volume and its anomaly percentage will show an exponential growth trend every 1-2 years, indicating that the Chaobai River basin has more extreme climate characteristics in recent years. The high-water period of the Chaobai River basin mainly occurs from July to December, and the normal water period of the basin is basically accompanied by the high-water period. However, in the past 12 years, the normal water period of the Chaohe River basin and the Baihe River basin has only occurred for 6 and 7 months respectively; The low water period covers most of the 12 years, and it is densely distributed in all periods except the high-water period and the normal water period. In all periods, the water volume of the Baihe River basin is higher than that of the Chaohe River basin, which may be attributed to the recharge of runoff by snow melting in spring. Based on the fine division of flow and wet and dry periods, the quantitative relationship between the wet and dry periods and water volume in the Chaobai River basin is established. The proportion of the wet and dry periods is the most important factor affecting the water volume in the basin. [Conclusion] The Chaobai River Basin has experienced an increase in extreme precipitation events in recent years, but the percentage of low water periods is much higher than normal water period and low water period。The relationship between the proportions of the three water periods is the most important factor influencing the change in water quantity in this watershed.

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  • 收稿日期:2023-11-13
  • 最后修改日期:2024-03-13
  • 录用日期:2024-03-13
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