中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
A Two-Source Normalized Soil Thermal Inertia Model for Estimating Field-Scale Soil Moisture from MODIS and ASTER Data

文献类型:期刊论文

作者Hao, Guibin1,2; Su, Hongbo3; Zhang, Renhua2; Tian, Jing2; Chen, Shaohui2
刊名REMOTE SENSING
出版日期2022-03-01
卷号14期号:5页码:20
关键词soil moisture soil thermal inertia ASTER MODIS remote sensing
DOI10.3390/rs14051215
通讯作者Su, Hongbo(hongbo@ieee.org)
英文摘要Soil moisture (SM) is a crucial component for understanding, modeling, and forecasting terrestrial water cycles and energy budgets. However, estimating field-scale SM based on thermal infrared remote-sensing data is still a challenging task. In this study, an improved Flexible Spatiotemporal DAta Fusion (FSDAF) method based on land-surface Diurnal Temperature Cycle (DTC) model (DFSDAF) was proposed to fuse Moderate Resolution Imaging Spectroradiometer (MODIS) and Advance Spaceborne Thermal Emission and Reflection Radiometer (ASTER) land-surface temperature (LST) data to generate ASTER-like LST during the night. The reconstructed diurnal LST data at a high spatial resolution (90 m) was then utilized to drive a two-source normalized soil thermal inertia model (TNSTI) for the vegetated surfaces to estimate field-scale SM. The results of the proposed methods were validated at different observation depths (2, 4, 10, 20, 40, 60, and 100 cm) over the Zhangye oasis in the middle region of the Heihe River basin in the northwest of China and were compared with the SM estimates from the TNSTI model and other SM products, including AMSR2/AMSR-E, GLDAS-Noah, and ERA5-land. The results showed the following: (1) The DFSDAF method increased the accuracy of LST prediction, with the determination coefficient (R-2) increasing from 0.71 to 0.77, and root mean square error (RMSE) decreasing from 2.17 to 1.89 K. (2) the estimated SMs had the best correlation with the observations at the 10 cm depth (with R-2 of 0.657; RMSE of 0.069 m(3)/m(3)), but the worst correlation with observations at the 40 cm depth (with R-2 of 0.262; RMSE of 0.092 m(3)/m(3)); meanwhile, the modeled SMs were significantly underestimated above 40 cm (2, 4, 10, and 20 cm) and slightly overestimated below 40 cm (60 and 100 cm); in addition, the field-scale SM series at high spatial resolution (90 m) showed significant spatiotemporal variation. (3) The SM estimates based on the TNSTI for the vegetated surfaces are more capable of characterizing the SM status in the root zone (~80 cm) or even deeper, while the SMs from AMSR2/AMSR-E, GLDAS-Noah, or ERA5-land products are closer to the SM in the surface layer (the depth is less than 5 cm). The TNSTI provided favorable data supports for hydrological model simulations and showed potential advantages for agricultural refinement managements and smart agriculture.
WOS关键词HEAT-FLUX ; AMSR-E ; RETRIEVAL ; TEMPERATURE ; SATELLITE ; ALGORITHM ; DROUGHT ; IMAGES ; VEGETATION ; RADIOMETER
资助项目National Natural Science Foundation of China[41971315/41571356/U2003105/42071327] ; National Key Research and Development Program of China[2021YFC3201102] ; National Aeronautics and Space Administration
WOS研究方向Environmental Sciences & Ecology ; Geology ; Remote Sensing ; Imaging Science & Photographic Technology
语种英语
WOS记录号WOS:000768262900001
出版者MDPI
资助机构National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Aeronautics and Space Administration
源URL[http://ir.igsnrr.ac.cn/handle/311030/172134]  
专题中国科学院地理科学与资源研究所
通讯作者Su, Hongbo
作者单位1.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China
3.Florida Atlantic Univ, Dept Civil Environm & Geomat Engn, Boca Raton, FL 33431 USA
推荐引用方式
GB/T 7714
Hao, Guibin,Su, Hongbo,Zhang, Renhua,et al. A Two-Source Normalized Soil Thermal Inertia Model for Estimating Field-Scale Soil Moisture from MODIS and ASTER Data[J]. REMOTE SENSING,2022,14(5):20.
APA Hao, Guibin,Su, Hongbo,Zhang, Renhua,Tian, Jing,&Chen, Shaohui.(2022).A Two-Source Normalized Soil Thermal Inertia Model for Estimating Field-Scale Soil Moisture from MODIS and ASTER Data.REMOTE SENSING,14(5),20.
MLA Hao, Guibin,et al."A Two-Source Normalized Soil Thermal Inertia Model for Estimating Field-Scale Soil Moisture from MODIS and ASTER Data".REMOTE SENSING 14.5(2022):20.

入库方式: OAI收割

来源:地理科学与资源研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。