2023
DOI: 10.3390/app13063916
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Algorithm for Retrieval of Temperature in Mesosphere and Lower Thermosphere from O2 A-Band Night Glow

Abstract: The O2 A-band night glow can be used to retrieve the temperature in the range of 80–120 km in the mesosphere and lower thermosphere (MLT). From the full spectrum of A-band night glow, the band used to retrieve temperature is selected based on the sensitivity of the emission line on temperature, taking into account the compromise relationship between the spectral band and resolution, inversion efficiency, and inversion accuracy. The non-linear iterative inversion method based on optimization theory is adopted f… Show more

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“…As an important tracer for the atmospheric photochemical and dynamical processes in the middle and upper atmosphere, the airglow is widely used to study the mechanisms of these processes due to the joint influence of atmospheric oscillations and external solar radiation (W. Wang et al, 2021;Xu et al, 2012;Yang et al, 2020). Oxygen molecules have seven electronic energy levels, which means the transition between different energy levels can produce airglow in different bands.…”
Section: Introductionmentioning
confidence: 99%
“…As an important tracer for the atmospheric photochemical and dynamical processes in the middle and upper atmosphere, the airglow is widely used to study the mechanisms of these processes due to the joint influence of atmospheric oscillations and external solar radiation (W. Wang et al, 2021;Xu et al, 2012;Yang et al, 2020). Oxygen molecules have seven electronic energy levels, which means the transition between different energy levels can produce airglow in different bands.…”
Section: Introductionmentioning
confidence: 99%