globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6276160
论文题名:
太湖西苕溪流域径流变化归因分析
其他题名: Attribution Analysis for Runoff Change in Xitiaoxi Basin
作者: 代晓颖; 许有鹏; 林芷欣; 王强; 徐羽; 袁甲
刊名: 长江流域资源与环境
ISSN: 1004-8227
出版年: 2018
卷: 27, 期:6, 页码:731-743
语种: 中文
中文关键词: 径流变化 ; 累积量斜率变化率 ; 气候弹性模型 ; 降水 ; 人类活动 ; 贡献率
英文关键词: runoff change ; the slope change ratio of cumulative quantity ; the climatic elasticity model ; precipitation ; human activities ; contribution ratio
WOS学科分类: GEOSCIENCES MULTIDISCIPLINARY
WOS研究方向: Geology
中文摘要: 气候变化与剧烈的人类活动正深刻地影响着全球水循环系统,河川径流作为水循环系统中的重要组成部分,也因此发生了显著的变化。为此,以太湖上游西苕溪流域为典型,应用累积距平、线性趋势分析及流量历时曲线等方法,分析1972 ~ 2015年流域内的水文气象变化趋势;基于累积量斜率变化分析方法与气候弹性模型,定量揭示降水与人类活动对流域径流变化的贡献率。研究结果显示: ( 1)1972 ~ 2015年间流域年径流量呈减小趋势,并且在1999年发生突变,以此将时间序列划分为基准期与变异期两个阶段。变异期流域年均径流量减少约11. 76%,减少幅度较大。( 2)流域降水量年际变化趋势并不显著,与基准期相比,变异期年均降水减少约1. 43%,减少幅度较小,但流域径流对降水变化敏感。汛期降水量占年降水量比重减少,降水的年内分配逐渐坦化,一定程度上使得产流减少。( 3)根据累积量斜率变化率分析方法,降水与人类活动对西苕溪流域径流减少的贡献率分别为26. 45%和73. 55%,由气候弹性模型计算得出二者的贡献率分别为23. 52%与76. 48%。两种计算方法结果较为接近,均表明人类活动是导致西苕溪流域径流减少的主要因素。
英文摘要: Climate change and intensive human activities had profound impacts on the global water circular system. As an important part in the water circular system,runoff changed significantly due to these two factors. Taking the Xitiaoxi Basin,which is located in the upper reaches of the Taihu Basin,as study area,the hydrological and meteorological trends in the Xitiaoxi Basin from 1972 to 2015 were analyzed by employing the accumulative anomaly,linear trend analysis and the flow duration curve method. Without considering the effect of evapotranspiration,the slope change ratio of cumulative quantity ( SCRCQ)method and the climatic elasticity model were adopted to estimate the impacts of precipitation and human activities on the runoff change quantitatively. The main results were showed as follows: ( 1)A decreasing trend of annual runoff was revealed during 1972-2015 in the Xitiaoxi Basin. An abrupt change was identified around the year 1999,then the entire period was divided into two parts: baseline period ( 1972-1998)and variable period ( 1999-2015). The annual runoff in the Xitiaoxi Basin decreased by 11. 76% or so after the occurrence of the abrupt change,which changed greatly. ( 2)The annual variation tendency of precipitation was not significant. Compared with the period before 1999,the annual average precipitation decreased by 1. 43% during 1999-2015,which changed lightly. The runoff in the Xitiaoxi Basin was very sensitive to the change of the precipitation. The proportion of the flood season precipitation in the annual precipitation has been declining and the seasonal distribution of precipitation gradually became smooth,which contributed to the runoff decrease in the Xitiaoxi Basin to a certain extent. ( 3)According to the slope change ratio of cumulative quantity method,the contribution ratios of the precipitation change and human activities were 26. 45% and 73. 55% respectively,while the results obtained by the climatic elasticity model were 23. 52% and 76. 48%. The results of these two methods were close and indicated that human activity was the main factor that led to the runoff decrease in the Xitiaoxi Basin during 1972-2015.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/155148
Appears in Collections:气候变化事实与影响

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作者单位: 南京大学地理与海洋科学学院, 南京, 江苏 210023, 中国

Recommended Citation:
代晓颖,许有鹏,林芷欣,等. 太湖西苕溪流域径流变化归因分析[J]. 长江流域资源与环境,2018-01-01,27(6):731-743
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