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An Overview of Inter-comparison Methodologies for Terra and Aqua MODIS Calibration

机译:Terra和Aqua MODIS校准的比对方法概述

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With increasing efforts on data fusion and long-term climate data records (CDR) using observations made by multiple sensors on the same or different platforms, sensor cross-calibration has become increasingly important. It is known that the uncertainty of climate models or science data records depends not only on the calibration quality of individual sensors but also on their calibration consistency. This paper provides an overview of inter-comparison methodologies applied by the MODIS Characterization Support Team (MCST) at NASA/GSFC for the studies of Terra and Aqua MODIS on-orbit calibration consistency. Improved over heritage sensors, MODIS was built with a set of on-board calibrators (OBC) that include a blackbody (BB), a space view (SV) port, a solar diffuser (SD), and a solar diffuser stability monitor (SDSM). The BB is primarily used for the thermal emissive bands (TEB) calibration and the SD/SDSM system for the reflective solar bands (RSB) calibration. Detector responses to the SV provide measurements for the instrument background. Although instrument design requirements and calibration approaches are nearly identical for both Terra and Aqua MODIS and they all went through extensive and similar pre-launch calibration and characterization activities, their on-orbit calibration consistency still has to be carefully examined and validated as many science products are generated from observations made by both instruments. Methodologies discussed in this paper include inter-comparison studies using the Moon, a third sensor, and ground targets. Our results show that Terra and Aqua reflective solar bands and thermal emissive bands have been calibrated consistently to within their combined uncertainty requirements. For the 11μm and 12μm bands used for surface temperature measurements, the calibration differences between Terra and Aqua MODIS are less than ±0.15K at scene temperatures from 240-280K and less than ±0.50K at cold scene temperatures from 190 to 230K (before corrections). For most reflective solar bands, their reflectance calibration differences are typically less than ±2%.
机译:随着对数据融合和长期气候数据记录(CDR)的使用越来越多的努力,使用在相同或不同平台上的多个传感器进行的观测,传感器交叉校准变得越来越重要。众所周知,气候模型或科学数据记录的不确定性不仅取决于单个传感器的校准质量,还取决于它们的校准一致性。本文概述了由NASA / GSFC的MODIS特征支持小组(MCST)应用的相互比较方法,以研究Terra和Aqua MODIS在轨校准一致性。与传统传感器相比,MODIS进行了改进,内置了一组车载校准器(OBC),其中包括黑体(BB),空间视图(SV)端口,太阳能扩散器(SD)和太阳能扩散器稳定性监视器(SDSM) )。 BB主要用于热发射带(TEB)校准,SD / SDSM系统用于反射太阳带(RSB)校准。检测器对SV的响应可提供仪器背景的测量结果。尽管Terra和Aqua MODIS的仪器设计要求和校准方法几乎相同,并且都经过了广泛且类似的发射前校准和表征活动,但与许多科学产品一样,仍必须仔细检查和验证其在轨校准一致性。是由两种仪器的观测结果生成的。本文讨论的方法包括使用月球,第三个传感器和地面目标进行的比对研究。我们的结果表明,Terra和Aqua反射太阳波段和热发射波段已被一致地校准到其综合不确定性要求之内。对于用于表面温度测量的11μm和12μm波段,在240-280K的场景温度下,Terra和Aqua MODIS之间的校准差异小于±0.15K,而在190至230K的寒冷场景温度下,其校准差异小于±0.50K(校正前) )。对于大多数反射性太阳能波段,其反射率校准差异通常小于±2%。

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