首页|近55年来气候变化和人类活动对增江径流变化影响的定量研究

近55年来气候变化和人类活动对增江径流变化影响的定量研究

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为探讨增江流域径流的变化特征及其对气候变化和人类活动的响应,选取1960-2015年河流实测径流量进行计算和分析.结果表明:56a年来,增江流域径流总体呈微弱增加趋势,每10 a增加0.6 mm,1960s径流量最少,2000s的径流量最多,1960-1972年为枯水期,1972-1984年为丰水期,1984-1991年为枯水期,此后至今一直为平水期.增江流域具有明显的丰枯季节变化,汛期流量占年径流总量的80%,径流总体呈明显的不对称双峰型,最大峰值出现在6月份,而次峰都出现在8月,夏季Cv值最小,冬季丰枯振荡最为明显.域内气候增暖明显,降雨量增加,蒸发量减少,下垫面参数n减小,对径流的增加十分有利.径流对各因子的敏感度绝对值为:最低气温>最高气温>降水>相对湿度>太阳辐射>LUCC>风速.气候变化和人类活动的多年平均贡献率分别为51.1%、48.9%.1980s后人类活动对径流影响程度大幅增加,2000s后人类活动影响减少,趋于缓和,人类正在努力和自然处于一种和谐平衡关系.因此,人类活动对径流变化的影响不容忽视.
The Runoff Variation of the Zengjiang River in Recent 55 Years and Quantitative Evaluations of the Impact of Climate Change and Human Activities
Based on the monthly runoff during 1960-2015,we have studied the characteristics and tendencies of the Zengjiang River and its response to the climate change and human activities.It shows that:over the past 56 years,the runoff of Zengjiang river has a slightly increasing tendency at a rate of 0.6 mm/lO a,and its volume dropped to the lowest in the 60s and reached the peak in the 2000s.The annual runoff of the river obviously decreased during 1960-1972,but shifted to increase during 1972-1984,and then turned to the declining trend again during 1960-1972.However,it stayed at its normal level till now.Runoff concentrates in the flood season by 80%,and presents obvious asymmetry bimodal type in several decades with a peak in June and a sub-peak in August.Runoff is affected by climate change and human activities.Runoff increases when climate is warmer and when precipitation increases,potential evapotranspiration decreases and LUCC is narrowed.The sensitivity of the runoff to the absolute value of various factors:Tmin>Tmax> Precipitation > Relative Humidity > Sunshine Duration >LUCC > Wind Speed.Climate change and human activities contribute to the runoff by 51.1% and 48.9% respectively.After 1980s,the influence of human activities on runoff increased drastically.But in the early 21st century,the influence of human activities reduced.Therefore,the contribution of human activities to the runoff change cannot be ignored.

Zengjiang River Basinrunoff variationclimate changehuman activitiesquantitative evaluation

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广东省水文局广州水文分局,广州510145

增江流域 径流变化 气候变化 人类活动 定量分析

2017

中国农村水利水电
水利部中国灌溉排水发展中心 水利部农村水电及电气化发展局 武汉大学 中国国家灌溉排水委员会

中国农村水利水电

CSTPCD北大核心
影响因子:0.655
ISSN:1007-2284
年,卷(期):2017.(11)
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