Improving the Calibration of Suomi NPP VIIRS Thermal Emissive Bands During Blackbody Warm-Up/Cool-Down

被引:16
|
作者
Wang, Wenhui [1 ]
Cao, Changyong [2 ]
Ignatov, Alexander [2 ]
Liang, Xingming [1 ]
Li, Zhenglong [3 ]
Wang, Likun [4 ]
Zhang, Bin [1 ,4 ]
Blonski, Slawomir [1 ]
Li, Jun [3 ]
机构
[1] Earth Resources Technol Inc, Laurel, MD 20707 USA
[2] NOAA, Ctr Satellite Applicat & Res, College Pk, MD 20740 USA
[3] Univ Wisconsin, Cooperat Inst Meteorol Satellite Studies, Madison, WI 53706 USA
[4] Univ Maryland, ESSIC, CICS, College Pk, MD 20740 USA
来源
关键词
Blackbody (BB) warm-up/cool-down (WUCD); radiometric calibration bias; sea surface temperature (SST) anomaly; sensor data record (SDR); Suomi National Polar-orbiting Partnership (S-NPP); thermal emissive bands (TEB); Visible Infrared Imaging Radiometer Suite (VIIRS);
D O I
10.1109/TGRS.2018.2870328
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 Suomi National Polar-orbiting Partnership Program Visible Infrared Imaging Radiometer Suite (VIIRS) thermal emissive hands (TEB) have been performing well during nominal operations since launch. However, small but persistent calibration anomalies are observed in all TEBs during the quarterly blackbody (BB) warm-up/cool-down (WUCD) events. As a result, the time series of daytime sea surface temperature (SST) (derived from bands M15-M16) show warm spikes on the order of 0.25 K. This paper suggests that VIIRS TEB WUCD biases are band dependent, with daily-averaged biases about -0.04 and 0.05 K for 14 and 15, and -0.05, -0.05, 0.11, 0.09, and 0.05 K for M12-M16, respectively. Two correction methods-Ltrace and WUCD-C-have been implemented and evaluated using colocated observations from the Cross-track Infrared Sounder (CrIS), radiative transfer simulations, and SST retrievals. Also an error in the National Oceanic and Atmospheric Administration operational processing was identified and fixed. Both correction methods effectively minimize WUCD-induced SST anomalies. The Ltrace method works well for I5, M12, and M14-M16, with residual biases about 0.01 K. The WUCD-C method, on the other hand, performs well to correct WUCD biases in all TEBs, with residual biases also about 0.01 K. How-ever, it introduces warm biases relative to CrIS at cold scene temperatures, which requires further study. Applying nonequal BB thermistor weights improves calibration at BB temperature set points, but its impact on daily-averaged WUCD biases is small. The proposed methodologies may also be applied to the VIIRS onboard the follow-on Joint Polar Satellite System satellites.
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页码:1977 / 1994
页数:18
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