普里皮亚季河流域河流状态的时空变化与气候变化

Budnik Svetlana Vasilivna
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引用次数: 1

摘要

在工作特点的普里皮亚季河流域的水文制度在气候变化的考虑。对某一地区气象特征的研究表明,该地区的气温、降水、水面和地面的蒸发量都有增加的趋势。这并没有明确地反映在水文特征、水域和领土对象的变化中。在河流的一部分水池中,河流的年中径流量在时间上有增长的趋势,而地下水位的变化在部分地区呈下降趋势——在这里,作为一种规则,在时间上倾向于与河流的年中径流量相反。河流中最高水温随时间的变化重复了河流中水流过程的趋势,即河流中水流增加时,最高温度增加,而减少时,最高温度降低。河流径流的表层成分的温度升高是由于所考虑的区域内空气温度的普遍升高而引起的。尽管大气降水数量增加,河流径流量增加或减少,但所有地区的泥沙带水量都在减少。径流层与降水、土壤湿度的关系具有一定的时滞。几乎所有站点的年平均水温随时间的变化都有上升的趋势,而河流最高水温随时间的变化具有多向的趋势,并且在更大程度上取决于河流水深的变化、最高水位的减少和频繁的解冻等。所进行的研究表明,在厚土层(0厘米-100厘米)中保持水分有助于增加河流的水流量,在乌克兰波列西河的现代条件下,这将解决为各种工业和人口提供高质量水资源的一些问题。
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Spatio-temporal Changes in the Regime of Rivers in the Pripyat River Catchment and Climate Change
In work features of a hydrological regime of catchments of the river of the Pripyat in climate change are considered. Researches of meteorological characteristics of the given territory show the tendency to growth, both temperatures of air, and precipitation, evaporation from a surface of water and ground also show the tendency to increase. That is not unequivocally reflected in change of a course of hydrological characteristics waters objects of territory. On a part of pools of the rivers the mid-annual runoff of water in the rivers in time tends to growth, and Change of levels of subsoil waters decreases for parts - on a turn - here, as a rule, tends a course in time opposite to a mid-annual runoff of water in the rivers. Change of the maximal temperature of water in the rivers in time repeats the tendency of a course of a runoff of water in them, i.e. at increase in a runoff of water in the rivers - the maximal temperature increases, and at reduction - decreases. The increase in temperature of a superficial component of a runoff of the rivers occurs because of the general increase in temperature of air in considered territory. Silt charge waters in all territory decreases, despite of increase in quantity of atmospheric precipitation and increases or reduction of a runoff of water in the rivers. The relationship between the water runoff layer and precipitation and soil moisture has a certain time delay. The average annual water temperature over time shows a tendency to increase at almost all stations, while the change in the maximum water temperature in rivers over time has a multidirectional tendency and to a greater extent depends on the change in water depth in the river, a decrease in high water maximums and frequent thaws, etc. The studies carried out show that the preservation of moisture in thick layers of soil (0 cm-100 cm) contributes to an increase in water flow in rivers and in the modern conditions of Polesie of Ukraine this will solve a number of problems with the provision of high-quality water resources for various industries and the population.
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