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A worldwide evaluation of basin-scale evapotranspiration estimates against the water balance method
Liu, WB (Liu, Wenbin)1; Wang, L (Wang, Lei)2,3; Zhou, J (Zhou, Jing)2; Li, YZ (Li, Yanzhong)1; Sun, FB (Sun, Fubao)1; Fu, GB (Fu, Guobin)4; Li, XP (Li, Xiuping)2; Sang, YF (Sang, Yan-Fang)1; Wang, L
Source PublicationJOURNAL OF HYDROLOGY
2016
Volume538Issue:0Pages:82-95
DOI10.1016/j.jhydrol.2016.04.006
AbstractEvapotranspiration (ET) plays a critical role in linking the water and energy cycles but is difficult to estimate at regional and basin scales. In this study, we present a worldwide evaluation of nine ET products (three diagnostic products, three land surface model (LSM) simulations and three reanalysis-based products) against reference ET (ETWb) calculated using the water balance method corrected for the water storage change at an annual time scale over the period 1983-2006 for 35 global river basins. The results indicated that there was no significant intra-category discrepancy in the annual ET estimates for the 35 basins calculated using the different products in 35 basins, but some products performed better than others, such as the Global Land surface Evaporation estimated using the Amsterdam Methodology (GLEAM_E) in the diagnostic products, ET obtained from the Global Land Data Assimilation System version 1 (GLDAS 1) with the Community Land Model scheme (GCLM_E) in LSM simulations, and ET from the National Aeronautics and Space Administration (NASA) Modern Era Retrospective-analysis for Research and Applications reanalysis dataset (MERRA_E) in the reanalysis-based products. Almost all ET products (except MERRA_E) reasonably estimated the annual means (especially in the dry basins) but systematically underestimated the inter-annual variability (except for MERRA_E, GCLM_E and ET simulation from the GLDAS 1 with the MOSAIC scheme - GMOS_E) and could not adequately estimate the trends (e.g. GCLM_E and MERRA_E) of ETwb, (especially in the energy-limited wet basins). The uncertainties in nine ET products may be primarily attributed to the discrepancies in the forcing datasets and model structural limitations. The enhancements of global forcing data (meteorological data, solar radiation, soil moisture stress and water storage changes) and model physics (reasonable consideration of the water and energy balance and vegetation processes such as canopy interception loss) will undoubtedly improve the estimation of global ET in the future. (C) 2016 The Authors. Published by Elsevier B.V.
Subject Area自然地理学
WOS IDWOS:000378360600008
Language英语
Indexed BySCI
KeywordGlobal Land Evapotranspiration Data Assimilation System River-basins Terrestrial Evapotranspiration Regional Evapotranspiration Complementary Relationship Groundwater Recharge Evaporation Model Precipitation
Cooperation Status国际
Department环境
Citation statistics
Cited Times:45[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/7671
Collection图书馆
Corresponding AuthorWang, L
Affiliation1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proces, Beijing 100101, Peoples R China
2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, 16 Lincui Rd, Beijing 100101, Peoples R China
3.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
4.CSIRO Land & Water, Private Bag 5, Wembley, WA 6913, Australia
Recommended Citation
GB/T 7714
Liu, WB ,Wang, L ,Zhou, J ,et al. A worldwide evaluation of basin-scale evapotranspiration estimates against the water balance method[J]. JOURNAL OF HYDROLOGY,2016,538(0):82-95.
APA Liu, WB .,Wang, L .,Zhou, J .,Li, YZ .,Sun, FB .,...&Wang, L.(2016).A worldwide evaluation of basin-scale evapotranspiration estimates against the water balance method.JOURNAL OF HYDROLOGY,538(0),82-95.
MLA Liu, WB ,et al."A worldwide evaluation of basin-scale evapotranspiration estimates against the water balance method".JOURNAL OF HYDROLOGY 538.0(2016):82-95.
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