DOI: 10.1029/2017JD028227
Scopus记录号: 2-s2.0-85048978197
论文题名: Temporal Characteristics of Actual Evapotranspiration Over China Under Global Warming
作者: Feng T. ; Su T. ; Ji F. ; Zhi R. ; Han Z.
刊名: Journal of Geophysical Research: Atmospheres
ISSN: 2169897X
出版年: 2018
卷: 123, 期: 11 起始页码: 5845
结束页码: 5858
语种: 英语
英文关键词: actual evapotranspiration
; Budyko hypothesis
; global warming
; reanalyses
Scopus关键词: climatic region
; data set
; evapotranspiration
; global warming
; hypothesis testing
; potential evapotranspiration
; regional climate
; temporal variation
; trend analysis
; China
英文摘要: In this study, an assessment is made of the trends of actual evapotranspiration (AE) over China under global warming from an ensemble of the following data sets: National Centers for Environmental Prediction-National Center for Atmospheric Research reanalysis I, National Centers for Environmental Prediction-Department of Energy reanalysis II, Modern-Era Retrospective Analysis for Research and Applications (MERRA), MERRA Version 2, European Centre for Medium-Range Weather Forecasts Interim Re-Analysis, and Japanese 55-year Reanalysis. For China as a whole, annual AE exhibited a significant increasing trend from 1979 to 2015, and the rate of increase was highest in autumn and lowest in summer. By subdividing China into six climatic regions using the aridity index, significant increasing trends in AE are found over the hyperarid, arid, and humid regions, but slightly decrease over the dry subhumid and subhumid regions. For the hyperarid and arid regions, the increases in potential evapotranspiration and the water supply from melting glaciers due to both climate warming and human activities might be the main contributors to the AE increases. An increase in potential evapotranspiration driven by global warming is the main cause of the increased AE over the humid region. On a seasonal basis, most AE over China occurs in summer. However, increasing AE trends have been observed mainly in autumn and winter, and the increase is statistically significant over all of China's six climatic regions in winter. In view of data availability, reanalyses are compared with the results from Mezentsev-Choudhury-Yang equation (AE_Budyko). The correlations between individual reanalyses and AE_Budyko tend to be higher over the arid region. ©2018. American Geophysical Union. All Rights Reserved. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/113723
Appears in Collections: 气候减缓与适应
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作者单位: College of Atmospheric Sciences, Lanzhou University, Lanzhou, China; College of Physical Science and Technology, Yangzhou University, Yangzhou, China; China Laboratory for Climate Studies, National Climate Center, China Meteorological Administration, Beijing, China
Recommended Citation:
Feng T.,Su T.,Ji F.,et al. Temporal Characteristics of Actual Evapotranspiration Over China Under Global Warming[J]. Journal of Geophysical Research: Atmospheres,2018-01-01,123(11)