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Spatial-temporal change analysis of evapotranspiration in the Heihe River Basin

机译:黑河流域蒸散量的时空变化分析。

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Evapotranspiration (ET) is one important component of hydrological process. It is also a limited factor for ecological environment conservation. The unreasonable utilization of water resources resulted in many problems in the Heihe River Basin, such as the over exploited of water resources, especial the ground water, the river flow decrease, land degradation. A correct understanding of the water consumption characteristics is undoubtedly a base of achieving the sustainable development of society, economy, and improving the eco-environment. In this paper, the time series of ET data estimated by ETWatch model which had been validated for different landscapes during the period of 2000–2010, were analyzed in spatial and temporal scales. The deviation of annual ET estimated by ETWatch with the observation ET data from eddy covariance system (EC) in the four observation stations of the basin was in the range of 5–8%. The conversion of land use type had a great impact on total water consumption across the basin due to lower variance of ET for three vegetation types. Base on the correlation analysis of climate factors and ET, there were apparent impact on ET in the upstream and midstream, but not in the downstream because of complicated human activities. The significant relations between temperature and ET (R=0.842∼0.941), and between precipitation and ET (R=0.582∼0.840), indicated that these two climate parameters were key influence factors on ET for grass land; The soil water storage was likely another influence factor on ET for the forest besides the temperature which had close relations with ET (R=0.617∼0.822). The spatial-temporal change analysis of ET and driven factors can be contributed to better understanding the eco-hydrological effect of the specific forest in Qilian Mountains.
机译:蒸散量(ET)是水文过程的重要组成部分。这也是保护生态环境的一个有限因素。水资源的不合理利用导致了黑河流域的许多问题,如水资源的过度开发,特别是地下水的开采,河流流量的减少,土地的退化。正确认识用水特征无疑是实现社会,经济可持续发展,改善生态环境的基础。本文对ETWatch模型估算的ET数据的时间序列进行了时空尺度分析,该序列已在2000–2010年期间针对不同景观进行了验证。 ETWatch与该盆地四个观测站的涡度协方差系统(EC)的观测ET数据估计的年度ET偏差在5-8%范围内。由于三种植被类型的ET变化较小,土地利用类型的转换对整个流域的总用水量有很大的影响。根据气候因素与ET的相关性分析,由于人类活动复杂,上游和中游对ET的影响明显,而下游没有。温度与ET之间的显着关系(R = 0.842〜0.941),降水与ET之间的显着关系(R = 0.582〜0.840)表明这两个气候参数是影响草地ET的关键因素。除了温度与ET密切相关外,土壤贮水量还可能是森林ET的另一个影响因素(R = 0.617〜0.822)。 ET和驱动因子的时空变化分析有助于更好地了解祁连山特定森林的生态水文效应。

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