首页> 外文期刊>Water >Separating the Impacts of Climate Variation and Human Activities on Runoff in the Songhua River Basin, Northeast China
【24h】

Separating the Impacts of Climate Variation and Human Activities on Runoff in the Songhua River Basin, Northeast China

机译:区分松花江流域气候变化和人类活动对径流的影响

获取原文
           

摘要

Climate variation and human activities are commonly recognized as two major factors affecting basin hydrology. However, quantifying their individual effect on runoff is challenging. In this study, long-term (1960–2009) river discharge and weather data in the Songhua River Basin (SRB, 556,800 km2), Northeast China, were gathered to separate the impacts of climate variation and human activities on runoff in five sub basins of the SRB. Mann-Kendall test, moving t-test and precipitation-runoff double cumulative curve were utilized to identify trends and change points of the hydrometeorlogical variables. Based on the change point, the 50-year study period was divided into two time series: 1960–1974 where minimal human activities took place and 1975–2009 where extensive land use change occurred and river engineering projects were undertaken. Subsequently, individual contributions of climate and human factors were assessed through a hydrologic sensitivity analysis. Our study found a significant decline in runoff of the SRB over the past 50 years. Contribution of climate variation and human activities to the change varied temporally and spatially. For the 1975–2009 period, human activities made a greater contribution (62%–82%) to the total runoff decline of the SRB. However, climate variation played a bigger role in runoff reduction in two sub river basins (63%–65%) between 1975 and 1989, as well as in runoff increase in other two sub river basins (85%–86%) between 1990 and 1999. Spatially, the effect of human activities on runoff decline was relatively stronger in the lower basin areas in the 1960s and 1970s while showing an increasing role in the upper basin areas in the past two decades.
机译:人们普遍认为气候变化和人类活动是影响流域水文学的两个主要因素。但是,量化它们对径流的影响是具有挑战性的。本研究收集了中国东北松花江流域(SRB,556,800 km 2 )的长期(1960-2009年)河流流量和天气数据,以区分气候变化和气候变化的影响。 SRB五个子流域的径流人类活动。利用Mann-Kendall检验,移动t检验和降水径流双累积曲线确定水文气象变量的趋势和变化点。根据变化点,将50年的研究期分为两个时间序列:1960–1974年,人类活动最少,而1975–2009年,土地用途发生了广泛变化,并进行了河流工程项目。随后,通过水文敏感性分析评估了气候和人为因素的个人贡献。我们的研究发现,在过去的50年中,SRB的径流量显着下降。气候变化和人类活动对变化的贡献随时间和空间而变化。在1975–2009年期间,人类活动对SRB的总径流量下降做出了更大的贡献(62%–82%)。但是,在1975年至1989年之间,气候变化在两个子流域的径流减少中发挥了更大的作用(63%–65%),在1990年到1990年之间,在另外两个子流域的径流增加中(85%–86%)发挥了更大的作用。 1999年。在空间上,人类活动对径流量下降的影响在1960年代和1970年代在下流域地区相对较强,而在过去二十年中在上流域中的作用日益增强。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号