The database of SABER/TIMED satellite campaign includes the distributions of nighttime O, H and some other characteristics of mesosphere – lower thermosphere region which are retrieved from the measurements of OH* volume emission rate (near 2 μm), temperature and ozone. In the core of the retrieval procedure lies the assumption about photochemical equilibrium of nighttime ozone and airglow model that considers two excited states of OH (levels ν = 9, 8). In this work, a modified OH* model (with the rate constants updated according to contemporary publications) is used to retrieve O, H, OH, HO2 and the chemical heating rate at 80–100 km altitudes from to SABER/TIMED measurements in 2002–2021. It was found that the use of new parameters in the retrieval procedure leads to significant (up to 2 times or more) changes in the resulting spatial distributions of O, H and chemical heating rate, while the corresponding changes in OH and HO2 distributions are minor.
No takes yet. Share an insight, caveat, or question.
Kulikov et al. (2024) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: