Skip to content

Mars

Mars is a terrestrial planet with a thin CO₂ atmosphere, extreme diurnal and seasonal temperature swings, a low-pressure surface environment, and extensive polar CO₂ and water ice deposits. It is the primary target of the tform simulator.


Physical constants

All values from the NASA Mars Fact Sheet:

Property Symbol Value Unit
Mass \(M\) \(6.4171 \times 10^{23}\) kg
Mean radius \(R\) \(3\,389\,500\) m
Surface gravity \(g\) \(3.721\) m s⁻²
Sidereal rotation period — \(88\,642.66\) s (~24h 37m)
Orbital period — \(686.97\) Earth days
Semi-major axis \(a\) \(1.524\) AU
Orbital eccentricity \(e\) \(0.0934\) —
Axial tilt \(\varepsilon\) \(25.19°\) —

Current atmospheric state

Mars today has a surface pressure of approximately \(636\,\text{Pa}\) — less than 1% of Earth's \(101\,325\,\text{Pa}\). The atmosphere is \(\sim 95\%\) CO₂ with trace N₂, Ar, and O₂ (Mahaffy et al., 2013):

Species Volume mixing ratio
CO₂ 95.32%
N₂ 2.60%
Ar 1.93%
O₂ 0.13%
CO 0.08%

Mean surface temperature is approximately \(210\,\text{K}\) (\(-63°\text{C}\)), with diurnal swings of 60–100 K and seasonal swings driven by CO₂ cap cycling.

The implementation uses MARS_ROTATION_PERIOD = 88775.244 s as its model sol and MARS_ORBITAL_PERIOD = 59356800 s (about 668.62 model sols). These differ from the sidereal rotation value in the fact-sheet table; use the model constants when reproducing its clock and timestep settings.


Mars in tform

The 3-D GCM is the primary model. It evolves spatial circulation, atmospheric/surface temperature, pressure and frost over MOLA terrain. Start with GCM setup and read validation limits. The torch global-mean model and its injection workflows are deprecated.

Topic Page
Solar flux and zenith angle model Solar Flux
Spatial dynamics and column physics Climate Model
Deprecated global-mean GHG injection GHG Interventions
API reference Mars API
Architecture Mars Architecture

Further reading