Implementation of evapotranspiration data assimilation with catchment scale distributed hydrological model via an ensemble Kalman Filter
Zou, Lei1; Zhan, Chesheng2; Xia, Jun1; Wang, Tiejun3; Gippel, Christopher J.4
刊名JOURNAL OF HYDROLOGY
2017-06-01
卷号549页码:685-702
关键词Evapotranspiration Data assimilation DTVGM-ET Ensemble Kalman Filter Huai River Basin
ISSN号0022-1694
DOI10.1016/j.jhydrol.2017.04.036
通讯作者Zhan, Chesheng(zhancs@igsnrr.ac.cn) ; Xia, Jun(xiajun666@whu.edu.cn)
英文摘要Terrestrial actual evapotranspiration (ETa) is a crucial component of terrestrial water cycles. The most common methods of estimating catchment-scale ETa are remote sensing and hydrological models. These methods have limitations when applied at the catchment scale due to coarse resolutions of data and uncertainties in model predictions. Data assimilation techniques that combine complementary information from hydrological models and observed data can overcome some of the limitations. These techniques have been used in many hydrological modeling studies, but few have applied data assimilation to ETa within a distributed precipitation-runoff catchment modeling framework. This paper proposes a catchment scale ETa data assimilation technique (termed ET-DA) that assimilates remotely sensed ETa data into a distributed time-variant gain hydrological model (DTVGM-ET) for improving hydrological model simulations. The DTVGM-ET improved the ETa computation on the basis of a nonlinear soil water availability function to establish an explicit time response relationship between ETa and soil moisture for implementing the ETa assimilation. The proposed ET-DA system was tested in the Upper Huai River Basin (UHRB), China using data from 2000 to 2012. Through synthetic simulation experiments, the capability of ET-DA for obtaining accurate, continuous time series of ETa estimates and achieving assimilation feedback on soil moisture and streamflow was examined. The results demonstrated that ET-DA provided improved regional ETa monitoring capability, and assimilation of ETa into the hydrological model led to improved model predictions of soil moisture and streamflow. (C) 2017 Elsevier B.V. All rights reserved.
资助项目National Grand Science and Technology Special Project of Water Pollution Control and Improvement of China[2014ZX07204-006] ; Key Research and Development Program of China[2015CB452701] ; National Natural Science Foundation of China[41571019] ; National Natural Science Foundation of China[41371043]
WOS关键词SENSED SOIL-MOISTURE ; WATER-BALANCE ; HEAT-FLUX ; MODIS ; STREAMFLOW ; EVAPORATION ; VALIDATION ; PRODUCTS ; STATES ; UNCERTAINTY
WOS研究方向Engineering ; Geology ; Water Resources
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000403855500053
资助机构National Grand Science and Technology Special Project of Water Pollution Control and Improvement of China ; Key Research and Development Program of China ; National Natural Science Foundation of China
内容类型期刊论文
源URL[http://ir.igsnrr.ac.cn/handle/311030/63129]  
专题中国科学院地理科学与资源研究所
通讯作者Zhan, Chesheng; Xia, Jun
作者单位1.Wuhan Univ, State Key Lab Water Resources & Hydropower Engn S, Wuhan 430072, Peoples R China
2.Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
3.Tianjin Univ, Inst Surface Earth Syst Sci, Tianjin 300072, Peoples R China
4.Griffith Univ, Australian Rivers Inst, Nathan, Qld 4111, Australia
推荐引用方式
GB/T 7714
Zou, Lei,Zhan, Chesheng,Xia, Jun,et al. Implementation of evapotranspiration data assimilation with catchment scale distributed hydrological model via an ensemble Kalman Filter[J]. JOURNAL OF HYDROLOGY,2017,549:685-702.
APA Zou, Lei,Zhan, Chesheng,Xia, Jun,Wang, Tiejun,&Gippel, Christopher J..(2017).Implementation of evapotranspiration data assimilation with catchment scale distributed hydrological model via an ensemble Kalman Filter.JOURNAL OF HYDROLOGY,549,685-702.
MLA Zou, Lei,et al."Implementation of evapotranspiration data assimilation with catchment scale distributed hydrological model via an ensemble Kalman Filter".JOURNAL OF HYDROLOGY 549(2017):685-702.
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