The Impact of Satellite Soil Moisture Data Assimilation on the Hydrological Modeling of SWAT in a Highly Disturbed Catchment

被引:0
|
作者
Liu, Yongwei [1 ]
Cui, Wei [2 ]
Ling, Zhe [3 ]
Fan, Xingwang [1 ]
Dong, Jianzhi [4 ]
Luan, Chengmei [5 ]
Wang, Rong [1 ]
Wang, Wen [6 ]
Liu, Yuanbo [1 ]
机构
[1] Chinese Acad Sci, Key Lab Watershed Geog Sci, Nanjing Inst Geog & Limnol, Nanjing 210008, Peoples R China
[2] Nanjing Hydraul Res Inst, Nanjing 210029, Peoples R China
[3] Water Resources Dept Jiangsu Prov, Nanjing 210029, Peoples R China
[4] Tianjin Univ, Sch Earth Syst Sci, Tianjin 300072, Peoples R China
[5] Hydrol & Water Resources Invest Bur Jiangsu Prov, Nanjing 210027, Peoples R China
[6] Hohai Univ, State Key Lab Hydrol Water Resources & Hydraul Eng, Nanjing 210098, Peoples R China
基金
国家重点研发计划;
关键词
soil moisture; data assimilation; SWAT; a disturbed catchment; ENSEMBLE KALMAN FILTER; STREAMFLOW OBSERVATIONS; PARAMETER-ESTIMATION; ERS SCATTEROMETER; SURFACE; UNCERTAINTY; SIMULATION; PREDICTION; STATES; CALIBRATION;
D O I
10.3390/rs16020429
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The potential of satellite soil moisture (SM) in improving hydrological modeling has been addressed in synthetic experiments, but it is less explored in real data cases. Here, we investigate the added value of Soil Moisture and Passive (SMAP) and Advanced Scatterometer (ASCAT) SM data to distributed hydrological modeling with the soil and water assessment tool (SWAT) in a highly human disturbed catchment (126, 486 km(2)) featuring a network of SM and streamflow observations. The investigation is based on the ensemble Kalman filter (EnKF) considering SM errors from satellite data using the triple collocation. The assimilation of SMAP and ASCAT SM improved the surface (0-10 cm) and rootzone (10-30 cm) SM at >70% and > 50% stations of the basin, respectively. However, the assimilation effects on distributed streamflow simulation of the basin are un-significant and not robust. SM assimilation improved the simulated streamflow at two upstream stations, while it deteriorated the streamflow at the remaining stations. This can be largely attributed to the poor vertical soil water coupling of SWAT, suboptimal model parameters, satellite SM data quality, humid climate, and human disturbance to rainfall-runoff processes. This study offers strong evidence of integrating satellite SM into hydrological modeling in improving SM estimation and provides implications for achieving the added value of remotely sensed SM in streamflow improvement.
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页数:18
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