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Logic Switches for MarTIM

SW5: True

SW6: True

SW8: True

Seasonal and global simulation options

Solar Activity: SMIN F10.7=67.2

EUV Efficiency: 23.0

Solar longitude: 180.0

Days to run: 5

Eddy Diffusion Coefficient: 1500.0m²s^-1

Switches to control the creation of output files from MarTIM

Output at the end of each simulation day: True

Wind files at the end of each simulation day: True

Volume mixing ratio files: True

Mass mixing ratio files: False

Momementum term files: False

Energy term files: False

Settings for when SW5 is true

Dust setting: SMIN plus Mars year 24 annually averaged dust (a typical Martian year in terms of atmospheric dust content as observed by Mars Global Surveyor during Mars year 24-25).

VMR Choice: False

TransMars Kinetic Configuration Options

Region for the kinetic code to simulate

Longitude range for kinetic code to simulate: 45.0 °

Photoabsorption subroutine output options

• Solar spectrum wavelength (nm), energies (eV) and photon fluxes (photons.cm⁻².s⁻¹). False
• Neutral species photoabsorption cross sections (cm⁻²) from the input files and interpolated onto the solar flux grid. False
• Ionization potentials (thresholds) (eV). False
• Normalized branching ratios and the number of difference photoionization excited states the different photoions can be photoionized to. False
• Neutral atmosphere - altitude (km), temperature (K) and neutral density (cm⁻³). False
• Photoelectron and individual photoion production rates (cm⁻³.s⁻¹) (summed over all solar flux energies) as a function of altitude (km) and subdivided into the contribution from individual excited ion states. False
• Photoelectron production rate (cm⁻³.s⁻¹.eV⁻¹) as a function of altitude and energy (eV) subdivided into the contribution from individual neutral atmosphere components. False
• Photoelectron production rate (cm⁻³.s⁻¹.eV⁻¹) summed over all neutrals as a function of altitude (km) and energy (eV). False
• Photoelectron and total photoion production rates (cm⁻³.s⁻¹.eV⁻¹) (summed over all solar flux energies) as a function of altitude and neutral specie (summation over all excited ion state per neutral specie). False

Boltzmann transport subroutine output options

• Upper boundary (user inputted) downward and upward precipitated electron flux (cm⁻².s⁻¹.eV⁻¹) as a function of energy (eV). False
• Total energy deposition per atmospheric layer (eV.cm⁻².s⁻¹). False
• Total inelastic collision cross-sections (cm⁻²) as a function of energy (eV) and subdivided by neutral specie. False
• Electron density (cm⁻³) as a function of altitude (km). False
• Elastic and inelastic collision cross-sections (cm⁻²) subdivided into individual collision states as a function of energy (eV). False
• Final production rates (total, primary, secondary, ions, electrons, neutral totals) (cm⁻³.s⁻¹) as a function of altitude (km). False
• Hemispheric energy flux (eV.cm⁻².s⁻¹) and particle flux (cm⁻².s⁻¹) as a function of altitude (km). False
• Energy deposited in the heating of ambient electrons (eV.cm⁻³s⁻¹) as a function of altitude (km). False
• Energy deposited in neutrals (eV.cm⁻³s⁻¹) as a function of altitude (km). False
• Excitation rates for the inelastic collision states of each neutral species (cm⁻³s⁻¹) as a function of altitude (km). False
• Precipitated electron energy and photoelectron energy integrated over energy and altitude (eV.cm⁻²s). False
• Electron-electron interaction loss function at each altitude (km) and energy (eV) grid point. False
• Excited ion production rates of each neutral species (cm⁻³s⁻¹) of each neutral species as a function of altitude (km). False
• Hemispheric upward and downward energy flux (eV.cm⁻².s⁻¹). False