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首页> 外文期刊>Applied Optics >Ground-based zenith sky abundances and in situ gas cross sections for ozone and nitrogen dioxide with the Earth Observing System Aura Ozone Monitoring Instrument
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Ground-based zenith sky abundances and in situ gas cross sections for ozone and nitrogen dioxide with the Earth Observing System Aura Ozone Monitoring Instrument

机译:借助地球观测系统Aura臭氧监测仪获取的臭氧和二氧化氮的地面天顶丰度和原位气体横截面

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摘要

High-accuracy spectral-slit-function calibration measurements, in situ ambient absorption gas cell measurements for ozone and nitrogen dioxide, and ground-based zenith sky measurements with the Earth Observing System Aura Ozone Monitoring Instrument (OMI) flight instrument are reported and the results discussed. For use of high-spectral-resolution gas absorption cross sections from the literature in trace gas retrieval algorithms, accurate determination of the instrument's spectral slit function is essential. Ground-based measurements of the zenith sky provide a geophysical determination of atmospheric trace gas abundances. When compared with other measurements, they can be used to verify the performance of the OMI flight instrument. We show that the approach of using published high-resolution absolute absorption cross sections convolved with accurately calibrated spectral slit functions for OMI compares well with in situ gas absorption cell measurements made with the flight instrument and that use of these convolved cross sections works well for reduction of zenith sky data taken with the OMI flight instrument for ozone and nitrogen dioxide that are retrieved from measured spectra of the zenith sky with the differential optical absorption spectroscopy technique, the same method to be used for the generation of in-flight data products. Finally, it is demonstrated that the spectral stability and signal-to-noise ratio performance of the OMI flight instrument, as determined from preflight component and full instrument tests, are sufficient to meet OMI mission objectives. © 2005 Optical Society of America.
机译:报告了高精度的光谱狭缝功能校准测量,臭氧和二氧化氮的原位环境吸收气室测量以及使用地球观测系统光环臭氧监测仪(OMI)飞行仪进行的地面天顶天空测量,并报告了结果讨论过。为了在痕量气体检索算法中使用文献中的高光谱分辨率气体吸收横截面,准确确定仪器的光谱狭缝功能至关重要。天顶天空的地面测量提供了大气中痕量气体丰度的地球物理测定。当与其他测量值进行比较时,它们可用于验证OMI飞行仪表的性能。我们表明,使用已发布的高分辨率绝对吸收截面与OMI的精确校准的光谱狭缝函数进行卷积的方法与使用飞行仪进行的原位气体吸收池测量结果比较,并且使用这些卷积横截面可以很好地减少使用OMI飞行仪获取的臭氧和二氧化氮的天顶数据,这些数据是通过差分光学吸收光谱技术从天顶的实测光谱中获取的,该方法与用于生成飞行中数据产品的方法相同。最后,证明了由飞行前组件和完整的仪器测试确定的OMI飞行仪器的频谱稳定性和信噪比性能足以满足OMI任务目标。 &复制; 2005年美国眼镜学会。

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