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首页> 外文期刊>Journal of geographical sciences >The dynamic variation of water resources and its tendency in the Tarim River Basin
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The dynamic variation of water resources and its tendency in the Tarim River Basin

机译:塔里木河流域水资源动态变化及其趋势。

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摘要

The method of time series is applied to analyze the variation of precipitation and temperature from 1961 to 2002 in the mountainous areas of the Tarim River Basin, as well as water consumption in the headstream and mainstream areas. Those hydrologic parameters are verified. Quantitative results indicate that the precipitation and temperature in the headstream areas have an increasing trend to different extent. The increasing trend of precipitation is less significant than that of the temperature (α= 0.05). Runoff of three headstreams also increases especially from 1994 to 2002. Compared with the perennial runoff, the annual runoff has increased by 25.163 X 10~8 m~3/a. However, inflows of the mainstream areas has only increased by 0.9985 X 10~8 m~3/a. So the runoff at the different hydrologic stations in the headstream areas has a linear decreasing trend. It is shown that the degraded trend of eco-environment of the Tarim River Basin hardly changes in the special water period for ten consecutive years. Given runoff of three headstreams is accounted in normal period from 1957 to 2003, the annual runoff of the headstream areas would be only 22.57 X 10~8 m~3. Therefore, more attention should be given to ecological safety of the Tarim River Basin.
机译:应用时间序列方法分析了塔里木河流域山区1961-2002年的降水和温度变化,以及源头和主流地区的耗水量。这些水文参数已得到验证。定量结果表明,上游地区的降水和温度有不同程度的上升趋势。降水的增加趋势不如温度的显着(α= 0.05)。特别是从1994年到2002年,三个源头的径流量也有所增加。与多年生径流相比,年径流量增加了25.163 X 10〜8 m〜3 / a。然而,主流地区的流入量仅增加了0.9985 X 10〜8 m〜3 / a。因此,上游地区不同水文站的径流量呈线性下降趋势。结果表明,塔里木河流域生态环境的退化趋势在特殊的水持续期连续十年几乎没有变化。从1957年到2003年的正常时期,考虑到三个源头的径流量,源头地区的年径流量仅为22.57 X 10〜8 m〜3。因此,应更加关注塔里木河流域的生态安全。

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