Temporal and Spatial Distribution of Evapotranspiration and Its Influencing Factors on Qinghai-Tibet Plateau from 1982 to 2014
Cui Mingyue3; Wang Junbang1; Wang Shaoqiang1; Yan Hao4; Li Yingnian2
刊名Journal of Resources and Ecology
2019
卷号10期号:2页码:213
关键词实际蒸散 青藏高原 气候因子 时空分布
ISSN号1674-764X
英文摘要Evapotranspiration is the key driving factor of the earth’s water cycle,and an important component of surface water and energy balances.Therefore,it also reflects the geothermal regulation function of ecohydrological process.The Qinghai-Tibet Plateau is the birthplace of important rivers such as the Yangtze River and the Yellow River.The regional water balance is of great significance to regional ecological security.In this study,ARTS,a dualsource remote sensing evapotranspiration model developed on a global scale,is used to evaluate the actual evapotranspiration (ET) in the Qinghai-Tibet Plateau from 1982 to 2014,using meteorological data interpolated from observations,as well as FPAR and LAI data obtained by satellite remote sensing.The characteristics of seasonal.interannual and dynamic changes of evapotranspiration were analyzed.The rates at which meteorological factors contribute to evapotranspiration are calculated by sensitivity analysis and multiple linear regression analysis,and the dominant factors affecting the change of evapotranspiration in the Qinghai-Tibet Plateau are discussed.The results show that:(1) The estimated values can explain more than 80% of the seasonal variation of the observed values (R~2 = 0.80,P <0.001),which indicates that the model has a high accuracy.(2) The evapotranspiration in the whole year,spring,summer and autumn show significant increasing trends in the past 30 years,but have significant regional differences.Whether in the whole year or in summer,the southern Tibetan Valley shows a significant decreasing trend (more than 20 mm per 10 years),while the Ali,Lhasa Valley and Haibei areas show increasing trends (more than 10 mm per 10 years).(3) Sensitivity analysis and multiple linear regression analysis show that the main factor driving the interannual change trend is climate warming,followed by the non-significant increase of precipitation.However,vegetation change also has a considerable impact,and together with climate factors,it can explain 56% of the interannual variation of evapotranspiration (multiple linear regression equation R~2 = 0.56,P <0.001).The mean annual evapotranspiration of low-cover grassland was 26.9% of high-cover grassland and 21.1% of medium-cover grassland,respectively.Considering significant warming and insignificant wetting in the Qinghai-Tibet Plateau,the increase of surface evapotranspiration will threaten the regional ecological security at the cost of glacial melting water.Effectively protecting the ecological security and maintaining the sustainable development of regional society are difficult and huge challenges.
语种英语
内容类型期刊论文
源URL[http://ir.igsnrr.ac.cn/handle/311030/155409]  
专题中国科学院地理科学与资源研究所
作者单位1.Institute of Geographic Sciences and Natural Resources Research,Chinese Academy of Sciences
2.Northwest Institute of Plateau Biology,Chinese Academy of Sciences
3.School of the Earth Sciences and Resources,China University of Geosciences
4.National Meteorological Center,China Meteorological Administration
推荐引用方式
GB/T 7714
Cui Mingyue,Wang Junbang,Wang Shaoqiang,et al. Temporal and Spatial Distribution of Evapotranspiration and Its Influencing Factors on Qinghai-Tibet Plateau from 1982 to 2014[J]. Journal of Resources and Ecology,2019,10(2):213.
APA Cui Mingyue,Wang Junbang,Wang Shaoqiang,Yan Hao,&Li Yingnian.(2019).Temporal and Spatial Distribution of Evapotranspiration and Its Influencing Factors on Qinghai-Tibet Plateau from 1982 to 2014.Journal of Resources and Ecology,10(2),213.
MLA Cui Mingyue,et al."Temporal and Spatial Distribution of Evapotranspiration and Its Influencing Factors on Qinghai-Tibet Plateau from 1982 to 2014".Journal of Resources and Ecology 10.2(2019):213.
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