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Radiometric Calibration of the Solar Backscatter Ultraviolet Sounder and Validation of Ozone Profile Retrievals

机译:太阳反向散射紫外探测器的辐射定标和臭氧剖面反演的验证

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The Solar Backscatter Ultraviolet Sounder (SBUS) is one of the 11 main payload instruments onboard Feng Yun-3 (FY-3), the second generation of Chinese polar orbit meteorological satellites. This paper presents the results of SBUS instrument calibration, and data and product validation during the prelaunch and postlaunch periods. Topics include the instrument prelaunch calibration and characterization, in-orbit monitoring, validation of the ozone profiles retrieved from the FY-3 SBUS measurements, and an application of the retrievals to monitoring the 2011 Arctic ozone depletion. For the prelaunch calibration of SBUS, the estimated uncertainty of laboratory calibration is approximately 4.7%. The in-orbit solar irradiance measurements indicate that the diffuser reflectivity degraded approximately 15% for the 252-nm channel, and 3% to 5% for the other 11 channels during a 12-mo period. Using ozone vertical profiles retrieved from National Oceanic and Atmospheric Administration Solar Backscatter Ultraviolet (SBUV)/2s as a “truth,” the initial comparison of ozone profiles between FY-3 SBUS and SBUV/2s finds that the relative percent bias of the FY-3 SBUS with the SBUV/2 results is good. The averaged differences range over to $pm$7% for FY-3A SBUS and $pm$6% for FY-3B SBUS. The SBUS ozone profile retrievals reveal that the spring 2011 Arctic ozone depletion mainly resulted from a sharp ozone decrease in the upper troposphere to lower stratosphere, which accounts for 70% to 80% of the total ozone loss.
机译:太阳反向散射紫外测深仪(SBUS)是中国第二代极地轨道气象卫星-风云3号(FY-3)上11种主要有效载荷仪器之一。本文介绍了在启动前和发布后SBUS仪器校准的结果以及数据和产品验证的结果。主题包括仪器的发射前校准和表征,在轨监测,对从FY-3 SBUS测量中获取的臭氧剖面进行验证以及将其应用于监测2011年北极臭氧消耗的情况。对于SBUS的启动前校准,实验室校准的估计不确定性约为4.7%。在轨太阳辐照度测量表明,在12个月内,对于252 nm通道,漫反射器的反射率下降了大约15%,对于其他11个通道,其反射率下降了3%至5%。使用从美国国家海洋和大气管理局太阳紫外线反向散射(SBUV)/ 2s中获取的臭氧垂直剖面作为“真相”,FY-3 SBUS和SBUV / 2s之间的臭氧剖面初步比较发现,FY-3的相对百分比偏差3 SBUS与SBUV / 2效果很好。 FY-3A SBUS的平均差异为$ pm $ 7%,FY-3B SBUS的平均差异为$ pm $ 6%。 SBUS臭氧剖面资料显示,2011年春季北极消耗臭氧层的主要原因是对流层上层至平流层下层的臭氧急剧减少,占臭氧总损失的70%至80%。

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