Inter-Calibration of Passive Microwave Satellite Brightness Temperature Observations between FY-3D/MWRI and GCOM-W1/AMSR2

被引:0
|
作者
Xu, Zuomin [1 ]
Sun, Ruijing [2 ,3 ]
Wu, Shuang [1 ]
Shao, Jiali [2 ,3 ]
Chen, Jie [2 ,3 ]
机构
[1] Heilongjiang Meteorol Bur, Heilongjiang Ecometeorol Ctr, Harbin 150030, Peoples R China
[2] China Meteorol Adm, Natl Satellite Meteorol Ctr, Natl Ctr Space Weather, Key Lab Radiometr Calibrat & Validat Environm Sate, Beijing 100081, Peoples R China
[3] Innovat Ctr FengYun Meteorol Satellite FYSIC, Beijing 100081, Peoples R China
基金
国家重点研发计划;
关键词
FY-3D/MWRI; GCOM-W1/AMSR2; brightness temperature; calibration; AMSR-E; SOIL-MOISTURE; SEA; INTERCALIBRATION; RADIOMETER; WATER; LAND; SMMR;
D O I
10.3390/rs16020424
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Microwave sensors possess the capacity to effectively penetrate through clouds and fog and are widely used in obtaining soil moisture, atmospheric water vapor, and surface temperature measurements. Long time-series datasets play a pivotal role in climate change studies. Unfortunately, the lifespan of operational satellites often falls short of the needs of these extensive datasets. Hence, comparing and cross-calibrating sensors with similar configurations is paramount. The Microwave Radiation Imager (MWRI) onboard Fengyun-3D (FY-3D) is the latest generation of satellite-based microwave remote sensing instruments in China, and its data quality and application prospects have attracted widespread attention. To comprehensively assess the data quality of MWRI, a comparison of the orbital brightness temperature (TB) data between FY-3D/MWRI and Global Change Observation Mission 1st-Water (GCOM-W1)/Advanced Microwave Scanning Radiometer 2 (AMSR2) is conducted, and then a calibration model is established. The results indicate a strong correlation between the two sensors, with a correlation coefficient exceeding 0.9 across all channels. The mean bias ranges from -1.5 K to 0.15 K. Notably, the bias of vertical polarization is more pronounced than that of horizontal polarization. The TB distribution patterns and temporal evolutions are highly consistent for both sensors, particularly under snow and ice. The small intercepts and close-to-1 slopes obtained during calibration further demonstrate the minor data differences between the two sensors. However, the calibration process effectively reduces the existing errors, and the calibrated FY-3D/MWRI TB data are closer to GCOM-W1/AMSR2, with a mean bias approximately equal to 0 K and a correlation coefficient exceeding 0.99. The excellent consistency of the TB data between the two sensors provides a vital data basis for retrieving surface parameters and establishing long time-series datasets.
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页数:27
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