Nighttime OH and HO chemical equilibria in the mesosphere–lower thermosphere
MY Kulikov, MV Belikovich, AG Chubarov… - Atmospheric …, 2024 - acp.copernicus.org
Abstract At the altitudes of the mesosphere–lower thermosphere, OH and HO 2
play a significant role in many physicochemical processes. Thus, monitoring their …
play a significant role in many physicochemical processes. Thus, monitoring their …
Energetic particle precipitation influences global secondary ozone distribution
J Jia, LE Murberg, T Løvset, YJ Orsolini… - … Earth & Environment, 2024 - nature.com
The secondary ozone layer is a global peak in ozone abundance in the upper mesosphere-
lower thermosphere (UMLT) around 90-95 km. The effect of energetic particle precipitation …
lower thermosphere (UMLT) around 90-95 km. The effect of energetic particle precipitation …
Responses of the Mean Thermosphere Circulation, O/N2 Ratio and Ne to Solar and Magnetospheric Forcing From Above and Tidal Forcing From Below
JM Forbes, X Zhang, A Maute… - Journal of Geophysical …, 2024 - Wiley Online Library
The day‐to‐day variability (“weather”) associated with the diurnal‐and zonal‐mean (DZM)
circulation, O/N2 ratio and electron density (Ne) of the I‐T system due to tidal “forcing from …
circulation, O/N2 ratio and electron density (Ne) of the I‐T system due to tidal “forcing from …