Abstract:
Diffusive-photochemical model of Mars atmosphere is constructed in 0-400 km heights range. The model includes neutral atmosphere lock and ionosphere. In the model there is interaction between neutral and ionized atmosphere that is important for computation of concentrations of H and H<sub>2</sub>. The results are obtained which fits the observational data.
Fulltext:
https:/.../preprint.asp?id=1995-75&lg=r