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Martian Atmosphere Observation and Modeling

v1.074
The merged extended version of the model with bimodal dust bins for average dust core radiuses 0.03, 0.1, 0.3 and 1 mkm. Drag coefficient is 0.005. Richardson-based CN vertical diffusion. Molecular diffusion correction with water vapor accommodation coefficient and Knudsen number. It has an extended height up to 160 km and more detailed CO2 cycle, enabled gravity waves and H2O photodissociation in the upper atmosphere.

v1.058
The base version of the model with bimodal dust bins for average dust core radiuses 0.03, 0.1, 0.3 and 1 mkm. Drag coefficient is 0.005. Richardson-based CN vertical diffusion. Molecular diffusion correction with water vapor accommodation coefficient and Knudsen number. Constants: N0 large = 15 cm-3, H0 large = 10 km, N0 small = 30000 cm-3, H0 small = 6 km, veff, large = 0.35, Reff, small = 0.05 mkm, veff, small = 0.1.

v1.029
The base version from another branch. Still haven't water cycle, but have an extended height up to 160 km and more detailed CO2 cycle. Weak solar activity with the solar radio flux at 10.7 cm = 80 s.f.u.