中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Spatial and temporal changes in aridity index in northwest China: 1960 to 2010

文献类型:SCI/SSCI论文

作者Liu X. M. ; Zhang D. ; Luo Y. Z. ; Liu C. M.
发表日期2013
关键词reference evapotranspiration penman-monteith pan evaporation river-basin water sensitivity variables paradox trend
英文摘要Northwest China is the driest region in China and the regional climate fluctuated dramatically during the last century. Aridity index, as the ratio between potential evapotranspiration and precipitation, is a good indicator to represent regional climate character. In this study, the change and attribution of the aridity index was investigated in northwest China using the observed climate data from 80 national meteorological stations during 1960-2010. The spatial and temporal variabilities of the aridity index shows that the annual aridity index decreased significantly (P < 0.05) by 0.048 year(-1), indicating that northwest China became wetter from 1960 to 2010. A differentiation equation method was used to attribute the change in aridity index to climate variables. The results indicate that the aridity index was most sensitive to the change in precipitation, followed by vapor pressure, solar radiation, wind speed, and air temperature. Increase in air temperature should have led to an increase in aridity index, but this effect had been offset by the increase in precipitation and vapor pressure and the decrease in wind speed. Increasing precipitation, which contributed 91.7 % of the decrease in the aridity index, was the dominant factor to the decrease in the aridity index in northwest China from 1960 to 2010.
出处Theoretical and Applied Climatology
112
1-2
307-316
收录类别SCI
语种英语
ISSN号0177-798X
源URL[http://ir.igsnrr.ac.cn/handle/311030/30387]  
专题地理科学与资源研究所_历年回溯文献
推荐引用方式
GB/T 7714
Liu X. M.,Zhang D.,Luo Y. Z.,et al. Spatial and temporal changes in aridity index in northwest China: 1960 to 2010. 2013.

入库方式: OAI收割

来源:地理科学与资源研究所

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