Global Soil Moisture Retrievals From the Chinese FY-3D Microwave Radiation Imager

被引:26
|
作者
Kang, Chuen Siang [1 ]
Zhao, Tianjie [1 ]
Shi, Jiancheng [1 ]
Cosh, Michael H. [2 ]
Chen, Yingying [3 ]
Starks, Patrick J. [4 ]
Collins, Chandra Holifield [5 ]
Wu, Shengli [6 ]
Sun, Ruijing [6 ]
Zheng, Jingyao [7 ]
机构
[1] Chinese Acad Sci, Aerosp Informat Res Inst, State Key Lab Remote Sensing Sci, Beijing 100864, Peoples R China
[2] ARS, USDA, Beltsville, MD 20705 USA
[3] Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China
[4] Grazinglands Res Lab, El Reno, OK 73036 USA
[5] USDA ARS, Southwest Watershed Res Ctr, Tucson, AZ 85719 USA
[6] China Meteorol Adm, Natl Satellite Meteorol Ctr, Beijing 100081, Peoples R China
[7] Hohai Univ, Coll Hydrol & Water Resources, Nanjing 210098, Peoples R China
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2021年 / 59卷 / 05期
基金
中国国家自然科学基金;
关键词
FengYun-3D (FY-3D); passive microwave remote sensing; soil moisture; vegetation optical depth (VOD); X-band; BRIGHTNESS TEMPERATURES; SURFACE-ROUGHNESS; WATER-CONTENT; VEGETATION; EMISSION; SMAP; MODEL; VALIDATION; SMOS; RADIOMETRY;
D O I
10.1109/TGRS.2020.3019408
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The FengYun-3 (FY-3) series satellite is the second generation of Chinese polar-orbiting meteorological satellite missions. The FY-3D satellite was launched on November 2017 and has been providing valuable data for meteorological applications, including brightness temperature (T-B) data from the MicroWave Radiation Imager (MWRI). In this study, we developed a global soil moisture retrieval algorithm, based on the radiative transfer equation (RTE) for using the FY-3D MWRI T-B to continue the soil moisture record from FY-3 satellites. We adopted a new empirical model to compute vegetation water content (VWC) based on the leaf area index (LAI) and canopy height (H) for vegetation effects correction. The Q(p) model, which addresses the soil surface roughness effects using dual-polarization information, is then used for soil moisture retrieval. Validation of the FY-3D soil moisture was conducted with the in-situ data and the validation results showed encouraging accuracy over a variety of landcovers, with bias and unbiased root-mean-squared difference (ubRMSE) at or below the level of 0.06 m(3) . m(-3). Monthly averaged soil moisture products generated from FY-3D could represent the seasonal changes in soil moisture and show reasonable spatial distribution of soil moisture at a global scale.
引用
收藏
页码:4018 / 4032
页数:15
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