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气候变化和人类活动对径流影响的贡献分解

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为量化气候变化和人类活动对径流量影响的贡献率,以大清河流域内张坊水文站和西大洋水库站上游为例,选用1957-2000年气象数据和水文数据,通过累积距平分析和Mann-Kendall非参数检验,分为基准期1957-1968年(Ⅰ期)和两个评价期1969-1979年(Ⅱ期)、1980-2000年(Ⅲ期)3个时段,采用分离评判法分解气候变化和人类活动对径流量影响的贡献率.总体上,张坊站和西大洋水库站径流量均呈显著下降趋势.张坊站上游Ⅱ期和Ⅲ期人类活动对径流量影响的贡献率分别为20%和24%;气候变化对径流量影响的贡献率分别为80%和76%.西大洋水库站上游Ⅱ期和Ⅲ期人类活动对径流量影响的贡献率分别为13%和18%;气候变化对径流量影响的贡献率为87%和82%.可见气候变化仍然是影响径流量变化的主要因素,由于降雨量变化不明显,初步判断,降雨量变化对径流量影响可能较小,主要受蒸发、温度和太阳辐射等因素影响;人类活动对径流量影响贡献率有明显增加的趋势.
Quantitative Analysis of The Effect of Climate Change and Human Activities on Streamflow
In order to make the quantitative analysis of the impacts of climate change and human activities on streamflow,Zhangfang hydrological station and Xidayang reservoir hydrological station upstream watersheds were selected as research object in Daqing river basin.Based on the hydro-meteorological data during 1957-2000 years,accumulated departure analysis and Mann-Kendall methods,the runoff time series are divided into three periods:reference period 1957-1958 (Ⅰ period),evaluation period 1969-1979 (Ⅱ period) and 1980-2000(Ⅲ period).Separation evaluation method was applied to quantify the respective contribution of climate change and human activities to the streamflow of the area.Significantly decreasing trend can be identified in the observed streamflow data of the two watersheds:Human activities contributed 20% (Ⅱ period) and 24% (Ⅲ period) reduction in the streamflow of Zhangfang upstream watershed,and climate change' s contribution rate reached 80% (Ⅱ period) and 76% (Ⅲ period),respectively;Human activities contributed 13% (Ⅱ period) and 18% (Ⅲ period) reduction in the streamflow of Xidayang upstream watershed,and climate change' s contribution rate reached 87% (Ⅱ period) and 82% (Ⅲ period),respectively.Climate change was the main contributor to the reduction in streamflow.As the rainfall decreases slowly,the effects of rainfall on the reduction in streamflow may be small proportion,on the contrary,mainly due to evapotranspiration,temperature and solar radiation,etc.The contribution from human activities on the reduction in streamflow gradually increases.

climate changehuman activityseparation evaluation methodstreamflowcontribution rate

王振海、李传哲、于福亮、徐征和、赵娜娜

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济南大学资源与环境学院,山东济南250022

中国水利水电科学研究院流域水循环模拟与调控国家重点实验室,北京100038

河海大学水文水资源与水利工程科学国家重点实验室,江苏南京210098

武汉大学水资源与水电工程科学国家重点实验室,湖北武汉430072

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气候变化 人类活动 分离评判法 径流量 贡献率

国家自然科学基金中国水利水电科学研究院科研专项水利部公益性行业科研专项

512092251232201201115

2014

济南大学学报(自然科学版)
济南大学

济南大学学报(自然科学版)

CSTPCD北大核心
影响因子:0.441
ISSN:1671-3559
年,卷(期):2014.28(4)
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