Quantitative estimation of the impact of climate change on actual evapotranspiration in the Yellow River Basin, China

被引:89
作者
Liu, Qiang [1 ]
Yang, Zhifeng [1 ]
机构
[1] Beijing Normal Univ, State Key Lab Water Environm Simulat, Sch Environm, Beijing 100875, Peoples R China
基金
中国国家自然科学基金; 美国国家科学基金会;
关键词
Actual evapotranspiration; Climate changes; Temporal trend; The simple steady state model; Water resources; The Yellow River Basin; PAN EVAPORATION TRENDS; MEAN ANNUAL EVAPOTRANSPIRATION; AVERAGE ANNUAL STREAMFLOW; SPATIAL-DISTRIBUTION; UNITED-STATES; WATER; VARIABILITY; COMPLEMENTARY; AFFORESTATION; PRECIPITATION;
D O I
10.1016/j.jhydrol.2010.10.031
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The spatial distribution and temporal trends for actual evapotranspiration (ETa) reflect the combined effects of the climate soil and vegetation This study was conducted to investigate the influence of climatic change on ETa Using the simple two-parameter steady-state model (SPS model) ETa was calculated from precipitation and potential evapotranspiration (ETp) at 89 meteorological stations during 1961-2006 in the Yellow River Basin (YRB) China The spatial distribution of ETa was performed by means of Kriging method and the temporal trends of ETa were investigated by the least squares linear model (linear fitted model) the Mann-Kendall method (the M-K method) Kendall tau statistical method (Kendall tau method) and the causes for the variations were discussed by means of the detrended method and SPS model The results presented that (i) the spatial distribution of ETa as most of the YRB is water-limited presented a similar spatial pattern with precipitation which demonstrates decreasing trends from southeast to northwest (ii) negative trends for ETa were detected by both the linear fitted model and Kendall tau method and significant decreasing trends (at 95% confidence level) were detected in all regions of YRB (iii) the timings of abrupt changes detected by the M-K method was 1991 1979 1975 and 1978 in the upper middle lower region and whole YRB respectively and so the ETa during 1961-2006 was divided into two periods natural period and changed period (e g natural period (1961-1990) and changed period (1991-2006) in the upper region) and (iv) the influence of climatic change on ETa contributed to -3 10 x 10(9) m(3) -4 26 x 10(9) m(3) -15 68 x 10(9) m(3) and -16 62 x 10(9) m(3) between natural period and changed period in the upper region middle region lower region and whole basin of YRB respectively The trends of ELa ETp and precipitation reflected that ETa is controlled by precipitation rather than ETp especially the results presented an evidence for the Bouchet s complementary hypothesis in the middle region of YRB (c) 2010 Elsevier B V All rights reserved
引用
收藏
页码:226 / 234
页数:9
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