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Spatiotemporal analysis of precipitation trends under climate change in the upper reach of Mekong River basin

机译:湄公河流域上游气候变化下降水趋势的时空分析

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Precipitation anomalies have greatly affected eco-hydrological processes in the upper reach of the Mekong River. In this research, an integrated spatiotemporal decomposition analysis method was proposed for the identification of precipitation trends under climate change at the basin scale. This method was a comprehensive use of multiple environmental statistical analysis approaches, including the S-mode empirical orthogonal function analysis, the inverse distance weighted interpolation, the Mann-Kendall trend test, the linear regression and the weighted moving average. Results indicated that precipitation trends were mainly obtained by two spatial-temporal variation patterns resulting from the decomposition of the original precipitation field. The primary spatial pattern (more than 40% variances) indicated that the annual and seasonal precipitation in the entire basin had a common variation trend. Moreover, variability of precipitation increased to the largest in the central basin and gradually decreased from north to south. Accordingly, precipitation-sensitive areas were mainly located in the east-central basin. The associated temporal trends showed that annual precipitation increased slightly over 1960-2009, and decreased significantly at the 5% significance level since 2000. Spring precipitation increased significantly over the entire study period. The secondary spatial pattern extracted at least 15% of the variance and represented a north-south inverse-variation trend. The northern mountainous region was more sensitive to climate change. Temporal trend analysis showed that annual precipitation had an increasing trend in the northern region and a decreasing trend in the southern region. Precipitation in the northern region increased significantly at the 1% significance level in winter. The research results could form a basis for supporting basin-scale water resources management, especially in the mountainous basin. (C) 2013 Elsevier Ltd and INQUA. All rights reserved.
机译:降水异常极大地影响了湄公河上游的生态水文过程。在这项研究中,提出了一种综合的时空分解分析方法来识别流域尺度下气候变化下的降水趋势。该方法是多种环境统计分析方法的综合使用,包括S模式经验正交函数分析,反距离加权插值,Mann-Kendall趋势检验,线性回归和加权移动平均值。结果表明,降水趋势主要是由原始降水场分解产生的两个时空变化模式获得的。初步的空间格局(方差超过40%)表明,整个盆地的年降水和季节降水具有共同的变化趋势。此外,降水的变异性在中部盆地增加到最大,并从北向南逐渐减小。因此,对降水敏感的地区主要位于中东部盆地。相关的时间趋势表明,在1960-2009年期间,年降水量略有增加,并且自2000年以来以5%的显着性水平显着下降。在整个研究期间,春季降水量显着增加。次空间格局至少提取了15%的方差,并代表了南北反向变化趋势。北部山区对气候变化更为敏感。时间趋势分析表明,北部地区年降水量呈上升趋势,南部地区呈年下降趋势。冬季,北部地区的降水显着增加,为1%。研究结果可为支持流域规模水资源管理提供基础,特别是在山区流域。 (C)2013 Elsevier Ltd和INQUA。版权所有。

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  • 来源
    《Quaternary International》 |2016年第21期|137-146|共10页
  • 作者单位

    Beijing Normal Univ, Sch Environm, Minist Educ, Key Lab Water & Sediment Sci, Beijing 100875, Peoples R China|Minist Environm Protect, Policy Res Ctr Environm & Econ, Beijing 100029, Peoples R China;

    Beijing Normal Univ, Sch Environm, Minist Educ, Key Lab Water & Sediment Sci, Beijing 100875, Peoples R China|Beijing Normal Univ, Sch Environm, State Key Lab Water Environm Simulat, Beijing 100875, Peoples R China;

    Beijing Normal Univ, Sch Environm, State Key Lab Water Environm Simulat, Beijing 100875, Peoples R China|Univ Regina, Inst Energy Environm & Sustainable Communities, 120,2 Res Dr, Regina, SK S4S 7H9, Canada;

    Beijing Normal Univ, Sch Environm, Minist Educ, Key Lab Water & Sediment Sci, Beijing 100875, Peoples R China;

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