乌拉尔河流域水势的变化

Z. Sivokhip, V. M. Pavleychik, A. Chibilev
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引用次数: 0

摘要

通过分析乌拉尔河流域径流的年际变化和季节变化,确定了乌拉尔河流域水情的特殊性。已经确定的是,最近几十年来已经观察到季节性径流重新分配的趋势,表现为冬季径流份额的增加。通过对差积分曲线的分析,揭示了不同含水率的物相;共模径流波动的普遍存在表明气候因子在径流形成中起主导作用。草原地区河流状况的一个重要特征是流量的年内变化,这形成了极端的水文情况(低水位或高水位)。在乌拉尔河流域组织有效和环境安全用水时应考虑这些结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Changes in water regime of the River Ural basin
Based on the analysis of the annual and seasonal variability of river runoff, the specificity of the water regime of the Ural River basin has been determined. It has been established that in recent decades a trend of redistribution of seasonal runoff has been observed, expressed in an increase in the share of runoff during the winter. Based on the analysis of difference integral curves, phases of different water content were revealed; the prevalence of common-mode runoff fluctuations indicates the leading role of climatic factors of runoff formation. An important feature of the rivers regime of the steppe regions is the intra-annual variability of the flow, which forms extreme hydrological situations (low water or high water). The results should be considered when organizing effective and environmentally safe water use in the Ural River basin.
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