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Sediment change under climate changes and human activities in the Yuanjiang-Red River Basin

机译:元江—红河流域气候变化与人类活动下的泥沙变化

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摘要

Both the climate change and human activities are the major influence factors to the sediment change in mountainous rivers. Based on the over 40 years' record, suspended sediment loads (SSL) change at the Manhao gauging station in the lower reaches of Yuanjiang River (upper Red River). In this paper, the variation of the sediment and its drivers were analyzed through different methods such as synchronous data comparison, traditional correlation, linear regression, and Granger causality. The results show that (1) the general trend of the annual average sediment concentration (SSC) and SSL at Manhao station is increasing from the 1960s to the 1990s, and there is a quick change period after 1984; (2) the SSL and SSC at Manhao station, during different periods of the 1960s, 1970s, 1980s and 1990s, are 1.87, 2.49, 3.129 3.63 kg/m(3), and 28.7x 10(6), 40.3 x 10(6), 44.1 x 10(6), 60.3 x 10(6) t/a, respectively; (3) the correlation analysis and the Granger causality test proved that the climate changes in the catchment were the main driving factors to the sediment variation in the period of 1960s and 1990s, but the influence by the mountainous human actions on the sediment change is stronger than that by the local climate changes in the 1970s and 1980s; (4) the correlation between the sediment changes and the forest coverage change is negative, which further proves that the sediment changes are strongly affected by the human activities in the basin.
机译:气候变化和人类活动都是影响山区河流沉积物变化的主要因素。根据40多年的记录,Yuan江下游(红河上游)的Manhao计量站的悬浮泥沙负荷(SSL)发生了变化。本文通过同步数据比较,传统相关,线性回归和格兰杰因果关系等不同方法分析了沉积物及其驱动因素的变化。结果表明:(1)从1960年代到1990年代,Manhao站年平均沉积物浓度(SSC)和SSL的总体趋势呈上升趋势,1984年以后有一个快速变化时期; (2)满好站的SSL和SSC在1960年代,1970年代,1980年代和1990年代的不同时期分别为1.87、2.49、3.129 3.63 kg / m(3)和28.7x 10(6),40.3 x 10( 6),44.1 x 10(6),60.3 x 10(6)t / a; (3)相关性分析和格兰杰因果关系检验证明,集水区的气候变化是1960年代和1990年代期间泥沙变化的主要驱动因素,但是山区人类活动对泥沙变化的影响更大。比1970年代和1980年代的当地气候变化所造成的影响要大; (4)沉积物变化与森林覆盖率变化的相关性为负,进一步证明了沉积物变化受流域人类活动的强烈影响。

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