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Response of snow hydrological processes to a changing climate during 1961 to 2016 in the headwater of Irtysh River Basin, Chinese Altai Mountains

机译:阿尔泰山额尔齐斯河流域源水在1961年至2016年期间雪水文过程对气候变化的响应

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摘要

With changing climatic conditions and snow cover regime,regional hydrological cycle for a snowy basin will change and further available surface water resources will be redistributed.Assessing snow meltwater effect on runoff is the key to water safety,under climate warming and fast social-economic developing status.In this study,stable isotopic technology was utilized to analyze the snow meltwater effect on regional hydrological processes,and to declare the response of snow hydrology to climate change and snow cover regime,together with longterm meteorological and hydrological observations,in the headwater of Irtysh River,Chinese Altai Mountains during 1961-2015.The average δ18O values of rainfall,snowfall,meltwater,groundwater and river water for 2014-2015 hydrological year were-10.9%,-22.3%,-21.796,-15.796 and-16.0%,respectively.The results from stable isotopes,snow melting observation and remote sensing indicated that the meltwater effect on hydrological processes in Kayiertesi River Basin mainly occurred during snowmelt supplying period from April to June.The contribution of meltwater to runoff reached 58.1% during this period,but rainfall,meltwater and groundwater supplied 49.1%,36.9% and 14.0% of water resource to annual runoff,respectively.With rising air temperature and increasing snowfall in cold season,the snow water equivalent (SWE) had an increasing trend but the snow cover duration declined by about one month including 13-day delay of the first day and 17-day advancement of the end day during 1961-2016.Increase in SWE provided more available water resource.However,variations in snow cover timing had resulted in redistribution of surface water resource,represented by an increase of discharge percentage in April and May,and a decline in June and July.This trend of snow hydrology will render a deficit of water resource in June and July when the water resource demand is high for agricultural irrigation and industrial manufacture.
机译:随着气候条件和积雪状况的变化,一个多雪盆地的区域水文循环将发生变化,并且将进一步分配可用的地表水资源。评估融雪对径流的影响是水安全,气候变暖和社会经济快速发展的关键。在这项研究中,利用稳定的同位素技术来分析积雪融水对区域水文过程的影响,并宣布积雪水文学对气候变化和积雪状况的响应,以及长期的气象和水文观测,以及该地区的源头。 1961-2015年,阿尔泰山额尔齐斯河.2014-2015年水文学年的降水,降雪,融水,地下水和河水的平均δ18O值分别为-10.9%,-22.3%,-21.796,-15.796和-16.0%稳定同位素,雪融观测和遥感的结果表明,融水对开耶尔特斯河水文过程的影响流域主要发生在4〜6月的融雪补给期。在此期间,融水对径流的贡献达到58.1%,而降雨,融水和地下水分别为年径流提供了49.1%,36.9%和14.0%的水资源。在寒冷季节,气温升高和降雪量增加,雪水当量(SWE)呈上升趋势,但积雪持续时间减少了约一个月,包括第一天的延迟13天和末日的提前17天。 1961年至2016年.SWE的增加提供了更多的可用水资源。然而,积雪时间的变化导致地表水资源的重新分配,以4月和5月的排放百分比增加以及6月和7月的减少为代表。当农业灌溉和工业生产对水资源的需求很高时,雪水文学的趋势将在6月和7月导致水资源短缺。

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  • 来源
    《山地科学学报(英文版)》 |2017年第11期|2295-2310|共16页
  • 作者单位

    State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;

    State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;

    Chinese Academy of Sciences Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China;

    State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;

    State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;

    State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;

    University of Chinese Academy of Sciences, Beijing 100049, China;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 eng
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