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Spatial and Temporal Characteristics of Reference Evapotranspiration Trends in the Haihe River Basin, China

机译:海河流域参考蒸散量的时空特征。

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摘要

In this study, the spatial and temporal patterns of trends for reference evapotranspiration (RET) at 34 meteorological stations (between 1957 and 2007) in the Haihe River basin, China, were analyzed using the Mann-Kendall (MK) test and the Sen's method. To reveal the possible causes and main driving forces of the changing patterns of RET, the spatial distribution and temporal patterns of trends for four meteorological variables (i.e., temperature, wind speed, relative humidity, and sunshine duration) were examined for each station. In addition, partial relative analysis between RET and meteorological variables and a sensitivity analysis of RET to meteorological variables were conducted. The results show the following: First, the Haihe River basin is dominated by a significant decreasing MK trend in annual RET at > 95% confidence level, which is observed at most stations in the eastern and southern areas of the basin. There are no observed trends or significant increasing MK trends in annual RET in the western plateau. For the intra-annual variability of RET, similar spatial-changing patterns are only observed in summer. Second, there are no obvious trends in RET from the late 1950s to the early 1970s for the whole basin. However, opposite trends of RET in the plateau area are identified after the 1970s in comparison with those in the plain and mountain area of the Haihe River basin. These two trends become significant in the late 1990s. Third, wind speed and sunshine duration are recognized as the two major driving forces for the decreasing trends in RET. Relative humidity is mainly responsible for the increasing trends in the western Haihe River basin during recent decades.
机译:在这项研究中,使用Mann-Kendall(MK)检验和Sen方法分析了中国海河流域34个气象站(1957年至2007年之间)参考蒸散量(RET)的时空趋势。 。为了揭示RET改变模式的可能原因和主要驱动力,每个站点检查了四个气象变量(即温度,风速,相对湿度和日照持续时间)的空间分布和趋势的时间模式。此外,还进行了RET与气象变量之间的部分相对分析以及RET对气象变量的敏感性分析。结果表明以下几点:首先,海河流域的年RET的MK趋势显着下降,且置信度大于95%,这在该流域东部和南部的大多数站点都可以观察到。在西部高原,每年的RET中没有观察到趋势或MK趋势显着增加。对于RET的年内变化,仅在夏季观察到类似的空间变化模式。其次,从1950年代末到1970年代初,整个盆地的RET没有明显的趋势。但是,与海河流域的平原和山区相比,1970年代后高原地区的RET趋势相反。这两种趋势在1990年代后期变得十分重要。第三,风速和日照时间被认为是RET下降趋势的两个主要驱动力。相对湿度是近几十年来海河流域西部地区增长趋势的主要原因。

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  • 来源
    《Journal of hydrologic engineering》 |2011年第3期|p.239-252|共14页
  • 作者单位

    Associate Professor, State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing 210098,China (corresponding author);

    Professor, State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing 210098, China;

    Associate Professor, State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing 210098,China;

    Principal Scientist, CSIRO Mathematical and Information Sciences,Private Bag 5, Wembley, WA 6913, Australia;

    Associate Professor, State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing 210098,China;

    M.S. Graduate Student, State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing 210098,China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    reference evapotranspiration; mann-kendall test; partial relative analysis; sensitivity analysis; haihe river basin; china;

    机译:参考蒸散量;曼-肯德尔检验部分相对分析;敏感性分析;海河流域中国;

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