首页> 外文期刊>Journal of Hydrology >Evaluating the contributions of climate change and human activities to runoff in typical semi-arid area, China
【24h】

Evaluating the contributions of climate change and human activities to runoff in typical semi-arid area, China

机译:气候变化和人类活动对典型半干旱区径流的贡献评价

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

Climate change and human activities have been widely recognized as two major factors that deeply influenced hydrological processes. It has great importance to evaluate and identify the contributions among distinct driving factors, which could help carry out better regional water resources management regulation. In this study, we used the Variable Infiltration Capacity (VIC) model to quantify the contributions for different climatic variables and human activities to runoff in the Luanhe River basin (LRB) with semi-arid climate, northern China. Our intention is to detect the multiple impacts of climate change (CC), such as precipitation change (PC) and temperature rising (TR), and human activities (HA), including land use/ cover change (LUCC) and direct human activities (i.e., water withdrawal and inter-basin water diversion, DHA), on runoff variance. The "natural period" (1961-1979), "weak impact period" (1980-1997) and "strong impact period" (1998-2016) were divided based on the double-mass curves and Mann-Kendall's test of observed runoff data from 1961 to 2016. The results indicated that, 1) compared with climate change, human activities were the major factors decreasing the runoff,which contributed more than 60 to the runoff reduction in two impact periods; 2) the runoff variation affected by climate was ruled by the precipitation change positively and strongly, and the impacts of precipitation and temperature strengthened with time. 3) During the strong impact period, the direct human activities have presented the most contribution on runoff reduction, which may result from the water diversion and water withdrawal. The influence of LUCC on runoff was mainly due to the conversion between grassland and cropland. These results would be helpful for policymakers and researchers to better understand the responses of runoff to this changing environment conditions and provide implications for future water resources planning and management at the basin scale.
机译:气候变化和人类活动被广泛认为是深刻影响水文过程的两大因素。评估和识别不同驱动因素之间的贡献具有重要意义,有助于更好地开展区域水资源管理监管。本研究采用变入渗能力(VIC)模型,量化了不同气候变量和人类活动对中国北方半干旱气候的滦河流域径流的贡献。我们的目的是检测气候变化 (CC) 的多重影响,例如降水变化 (PC) 和温度上升 (TR),以及人类活动 (HA),包括土地利用/覆盖变化 (LUCC) 和直接人类活动(即取水和流域间引水,DHA),对径流方差的影响。根据双质量曲线和Mann-Kendall对1961—2016年径流观测资料的检验,划分了“自然期”(1961-1979)、“弱影响期”(1980-1997)和“强影响期”(1998-2016)。结果表明:(1)与气候变化相比,人类活动是减少径流的主要因子,对2个影响期径流减少的贡献率均超过60%;2)降水变化对气候影响的径流变化呈正向和强变化规律,降水和温度的影响随时间推移而增强。3)在强影响期,人类直接活动对径流减少的贡献最大,这可能是由于引水和取水造成的。LUCC对径流的影响主要归因于草地和耕地之间的转换。这些结果有助于政策制定者和研究人员更好地了解径流对这种变化环境条件的响应,并为未来流域尺度的水资源规划和管理提供启示。

著录项

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