中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Evaluation of evapotranspiration estimates for two river basins on the Tibetan Plateau by a water balance method

文献类型:期刊论文

作者Xue, Bao-Lin; Wang, Lei; Li, Xiuping; Yang, Kun; Chen, Deliang1; Sun, Litao3
刊名JOURNAL OF HYDROLOGY
出版日期2013
卷号492页码:290-297
ISSN号0022-1694
关键词Evapotranspiration Water balance method Global evapotranspiration product Tibetan Plateau
DOI10.1016/j.jhydrol.2013.04.005
文献子类Article
英文摘要Evapotranspiration (E) at regional or basin scale is difficult to estimate. This study estimates E with a water balance method for the upper Yellow River and Yangtze River basins on the Tibetan Plateau, where in situ data accessibility is especially insufficient. Results indicate that annual terrestrial water storage change in the two basins is negligible, and basin-scale E can be reliably estimated by the difference between precipitation and runoff. Thus, four E products from Zhang-(Zhang_E), MODIS (MODIS_E), Japanese 25-year reanalysis product (JRA_E), and the newly published Global Land Data Assimilation System with Noah Land Surface Model-2 (GLDAS_E)-are evaluated against E estimated by the water balance method. GLDAS_E and Zhang_E had the best performance for the upper Yellow River basin and Yangtze River basin, respectively, with relatively small underestimation. Further analysis showed that the underestimation of GLDAS_E was mainly caused by its negative bias for precipitation, whereas the overestimation of JRA_E was due to overestimation of downward shortwave radiation. MODIS_E greatly overestimated E in both basins, which was also caused by high downward shortwave radiation flux inputs from the Global Modeling and Assimilation Office. Thus, more accurate forcing data for these products should be a future focus, since they can improve E estimates, at least for the Tibetan Plateau. (C) 2013 Elsevier B.V. All rights reserved.
学科主题Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources
电子版国际标准刊号1879-2707
出版地AMSTERDAM
WOS关键词REGIONAL EVAPOTRANSPIRATION ; CLIMATE-CHANGE ; FOREST ; GRACE ; FORCINGS ; RUNOFF ; MODEL ; MODIS
WOS研究方向Science Citation Index Expanded (SCI-EXPANDED)
语种英语
出版者ELSEVIER
WOS记录号WOS:000321023900026
资助机构National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)) ; Hundred Talents Program of Chinese Academy of Sciences(Chinese Academy of Sciences) ; Strategic Priority Research Program of the Chinese Academy of Sciences(Chinese Academy of Sciences)
源URL[http://ir.ibcas.ac.cn/handle/2S10CLM1/28051]  
专题植被与环境变化国家重点实验室
作者单位1.Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing 100093, Peoples R China
2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China
3.Univ Gothenburg, Dept Earth Sci, Gothenburg, Sweden
4.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Xue, Bao-Lin,Wang, Lei,Li, Xiuping,et al. Evaluation of evapotranspiration estimates for two river basins on the Tibetan Plateau by a water balance method[J]. JOURNAL OF HYDROLOGY,2013,492:290-297.
APA Xue, Bao-Lin,Wang, Lei,Li, Xiuping,Yang, Kun,Chen, Deliang,&Sun, Litao.(2013).Evaluation of evapotranspiration estimates for two river basins on the Tibetan Plateau by a water balance method.JOURNAL OF HYDROLOGY,492,290-297.
MLA Xue, Bao-Lin,et al."Evaluation of evapotranspiration estimates for two river basins on the Tibetan Plateau by a water balance method".JOURNAL OF HYDROLOGY 492(2013):290-297.

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来源:植物研究所

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