中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The spatiotemporal variation of reference evapotranspiration and the contribution of its climatic factors in the Loess Plateau, China

文献类型:SCI/SSCI论文

作者Li Y. Z.; Liang, K.; Bai, P.; Feng, A. Q.; Liu, L. F.; Dong, G. T.
发表日期2016
关键词Reference evapotranspiration Climate factors contribution Climate change Loess Plateau key meteorological variables surface wind speeds yellow-river basin past 50 years pan-evaporation tibetan plateau potential evapotranspiration trend analysis aridity index sensitivity
英文摘要Reference evapotranspiration (ET0) is an important parameter of agricultural activity and hydrometeorological studies. In this study, we used the Food and Agriculture Organization Penman-Monteith equation to evaluate ET0, and to investigate the change point of ET0 in the Loess Plateau region from 1960 to 2013. The results showed that a change point was detected at approximately the year 1990 for annual ET0 series from 108 meteorological stations using Cramer's statistical test. The annual ET0 decreased significantly (p < 0.05) by -1.22 mm year -1 from 1960 to 1990, especially during the summer months, which contributed the most to the total annual reduction, while it increased significantly (p < 0.001) by 1.15 mm year -1 from 1991 to 2013, with the spring months contributing the most. The ET0 and its trend in the five integrated management divisions of the Loess Plateau have significant spatial heterogeneity. The highest and lowest ET0 were found in the third and fifth divisions from 1960 to 2013. The ET0 decreased significantly in the first division and increased in the fourth divisions (1960-1990 and 1991-2013, respectively). Using differential equations to quantitatively evaluate the contribution of various factors, the wind speed was mostly responsible for the variability in the ET0 trend from 1960 to 1990, followed by solar radiation and vapor pressure. The positive effect of air temperature on ET0 trend was offset by the other three factors, and the combined effects of the four climatic variables led to the decrease in the ET0 trend. However, the rapidly increasing air temperature became the predominant factor in the change in the ET0 trend after 1990. A spatiotemporal variation of pre-dominant contribution to the ET0 trend was identified. The temperature dominant region changed from the third to the first division for 1960-1990 and 1991-2013. Radiation did not change. Vapor pressure changed from the first to the fourth and the wind speed changed from the forth to the third. This study could contribute to a better understanding of the response of the spatial and temporal variation of ET0 to increased climate change. Additionally, this research also provides scientific support to regional planning and management.
出处Environmental Earth Sciences
75
4
语种英语
ISSN号1866-6280
DOI标识10.1007/s12665-015-5208-7
源URL[http://ir.igsnrr.ac.cn/handle/311030/43065]  
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
Li Y. Z.,Liang, K.,Bai, P.,et al. The spatiotemporal variation of reference evapotranspiration and the contribution of its climatic factors in the Loess Plateau, China. 2016.

入库方式: OAI收割

来源:地理科学与资源研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。