Hydroxyl layer: trend of number density and intra-annual variability
The layer of vibrationally excited hydroxyl (OH*) near the mesopause in Earth's atmosphere is widely used to derive the temperature at this height and to observe dynamical processes such as gravity waves. The concentration of OH* is controlled by the product of atomic hydrogen, with ozone cr...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2015-06-01
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Series: | Annales Geophysicae |
Online Access: | https://www.ann-geophys.net/33/749/2015/angeo-33-749-2015.pdf |