globalchange  > 气候变化与战略
DOI: 10.5194/hess-24-1485-2020
论文题名:
Evaluation of global terrestrial evapotranspiration using state-of-the-art approaches in remote sensing; machine learning and land surface modeling
作者: Pan S.; Pan N.; Tian H.; Friedlingstein P.; Sitch S.; Shi H.; Arora V.K.; Haverd V.; Jain A.K.; Kato E.; Lienert S.; Lombardozzi D.; Nabel J.E.M.S.; Ottlé C.; Poulter B.; Zaehle S.; Running S.W.
刊名: Hydrology and Earth System Sciences
ISSN: 1027-5606
出版年: 2020
卷: 24, 期:3
起始页码: 1485
结束页码: 1509
语种: 英语
Scopus关键词: Data fusion ; Deep learning ; Evapotranspiration ; Learning systems ; Remote sensing ; Surface measurement ; Interannual variability ; Land surface modeling ; Land surface models ; Relative stabilities ; Significance levels ; Spatial and temporal variation ; State-of-the-art approach ; Terrestrial evapotranspiration ; Learning algorithms ; algorithm ; anthropogenic effect ; evapotranspiration ; machine learning ; remote sensing ; spatiotemporal analysis ; terrestrial environment ; water stress ; Amazon Basin
英文摘要: Evapotranspiration (ET) is critical in linking global water, carbon and energy cycles. However, direct measurement of global terrestrial ET is not feasible. Here, we first reviewed the basic theory and state-of-the-art approaches for estimating global terrestrial ET, including remote-sensingbased physical models, machine-learning algorithms and land surface models (LSMs). We then utilized 4 remotesensing-based physical models, 2 machine-learning algorithms and 14 LSMs to analyze the spatial and temporal variations in global terrestrial ET. The results showed that the ensemble means of annual global terrestrial ET estimated by these three categories of approaches agreed well, with values ranging from 589.6 mm yr-1 (6.56 × 104 km3 yr-1) to 617.1 mm yr-1 (6.87 × 104 km3 yr-1). For the period from 1982 to 2011, both the ensembles of remote-sensing-based physical models and machine-learning algorithms suggested increasing trends in global terrestrial ET (0.62 mm yr-2 with a significance level of p < 0.05 and 0.38 mm yr-2 with a significance level of p < 0.05, respectively). In contrast, the ensemble mean of the LSMs showed no statistically significant change (0.23 mm yr-2, p > 0.05), although many of the individual LSMs reproduced an increasing trend. Nevertheless, all 20 models used in this study showed that anthropogenic Earth greening had a positive role in increasing terrestrial ET. The concurrent small interannual variability, i.e., relative stability, found in all estimates of global terrestrial ET, suggests that a potential planetary boundary exists in regulating global terrestrial ET, with the value of this boundary being around 600 mm yr-1. Uncertainties among approaches were identified in specific regions, particularly in the Amazon Basin and arid/semiarid regions. Improvements in parameterizing water stress and canopy dynamics, the utilization of new available satellite retrievals and deep-learning methods, and model-data fusion will advance our predictive understanding of global terrestrial ET. © Author(s) 2020.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/162749
Appears in Collections:气候变化与战略

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作者单位: Pan, S., International Center for Climate and Global Change Research, School of Forestry and Wildlife Sciences, Auburn University, Auburn, AL 36832, United States; Pan, N., International Center for Climate and Global Change Research, School of Forestry and Wildlife Sciences, Auburn University, Auburn, AL 36832, United States, State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, China; Tian, H., International Center for Climate and Global Change Research, School of Forestry and Wildlife Sciences, Auburn University, Auburn, AL 36832, United States; Friedlingstein, P., College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, EX4 4QF, United Kingdom; Sitch, S., College of Life and Environmental Sciences, University of Exeter, Exeter, EX4 4RJ, United Kingdom; Shi, H., International Center for Climate and Global Change Research, School of Forestry and Wildlife Sciences, Auburn University, Auburn, AL 36832, United States; Arora, V.K., Canadian Centre for Climate Modelling and Analysis, Environment Canada, University of Victoria, Victoria, BC V8W 2Y2, Canada; Haverd, V., CSIRO Oceans and Atmosphere, GPO Box 1700, Canberra, ACT 2601, Australia; Jain, A.K., Department of Atmospheric Sciences, University of Illinois, Urbana, IL 61801, United States; Kato, E., Institute of Applied Energy (IAE), Minato-ku, Tokyo, 105-0003, Japan; Lienert, S., Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland; Lombardozzi, D., Climate and Global Dynamics Laboratory, National Center for Atmospheric Research, Boulder, CO 80305, United States; Nabel, J.E.M.S., Max Planck Institute for Meteorology, Bundesstr. 53, Hamburg, 20146, Germany; Ottlé, C., LSCE-IPSL-CNRS, Orme des Merisiers, Gif-sur-Yvette, 91191, France; Poulter, B., NASA Goddard Space Flight Center, Biospheric Sciences Laboratory, Greenbelt, MD 20771, United States; Zaehle, S., Max Planck Institute for Biogeochemistry, P.O. Box 600164, Hans-Knöll-Str. 10, Jena, 07745, Germany; Running, S.W., Numerical Terradynamic Simulation Group, College of Forestry and Conservation, University of Montana, Missoula, MT 59812, United States

Recommended Citation:
Pan S.,Pan N.,Tian H.,et al. Evaluation of global terrestrial evapotranspiration using state-of-the-art approaches in remote sensing; machine learning and land surface modeling[J]. Hydrology and Earth System Sciences,2020-01-01,24(3)
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