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通过大气痕量分子光谱实验从太空对太阳红外光谱进行的观测。

Observations of the infrared solar spectrum from space by the ATMOS experiment.

作者信息

Abrams M C, Goldman A, Gunson M R, Rinsland C P, Zander R

出版信息

Appl Opt. 1996 Jun 1;35(16):2747-51. doi: 10.1364/AO.35.002747.

Abstract

The final flight of the Atmospheric Trace Molecule Spectroscopy experiment as part of the Atmospheric Laboratory for Applications and Science (ATLAS-3) Space Shuttle mission in 1994 provided a new opportunity to measure broadband (625-4800 cm(-1), 2.1-16 µm) infrared solar spectra at anunapodized resolution of 0.01 cm(-1) from space. The majority of the observations were obtained as exoatmospheric, near Sun center, absorption spectra, which were later ratioed to grazing atmospheric measurements to compute the atmospheric transmission of the Earth's atmosphere and analyzed for vertical profiles of minor and trace gases. Relative to the SPACELAB-3 mission that produced 4800 high Sun spectra (which were averaged into four grand average spectra), the ATLAS-3 mission produced some 40,000 high Sun spectra (which have been similarly averaged) with an improvement in signal-to-noise ratio of a factor of 3-4 in the spectral region between 1000 and 4800 cm(-1). A brief description of the spectral calibration and spectral quality is given as well as the location of electronic archives of these spectra.

摘要

作为1994年大气应用与科学实验室(ATLAS - 3)航天飞机任务的一部分,大气痕量分子光谱实验的最后一次飞行提供了一个新机会,可从太空以0.01 cm⁻¹的未变迹分辨率测量宽带(625 - 4800 cm⁻¹,2.1 - 16 µm)红外太阳光谱。大部分观测数据是作为外大气层、接近太阳中心的吸收光谱获取的,这些光谱后来与掠射大气测量数据进行比值计算,以得出地球大气层的大气透过率,并分析微量和痕量气体的垂直分布。相对于产生了4800条高太阳光谱(平均为四条总平均光谱)的空间实验室 - 3任务,ATLAS - 3任务产生了约40,000条高太阳光谱(同样进行了平均),在1000至4800 cm⁻¹光谱区域的信噪比提高了3至4倍。文中还简要介绍了光谱校准和光谱质量,以及这些光谱的电子存档位置。

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