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Table 2
Input datasets for fitting the CO2 region around 4.27 μm.
| Detailed description | Rocha model | Trivial name for Table 3 |
|---|---|---|
| H2O/CO2/NH3/CH4 72 K absorbance | D13a | Warm absorption |
| H2O/CO2/NH3/CH4 35 K absorbance | D12a | Lukewarm absorption |
| H2O/CO2 13 K absorbance | D2a | Cold absorption |
| CO2 13 K absorbance | G2 | Cold absorption pure CO2 |
| MgSiO3/H2O 100 K core + D13a 72 K mantle scatter | D13a | Warm scattering |
| MgSiO3/H2O 10 K core + D12a 35 K mantle scatter | D12a | Lukewarm scattering |
| MgSiO3/H2O 10 K core + D2a 13 K mantle scatter | D2a | Cold scattering |
| MgSiO3/H2O 10 K core + G2 13 K mantle scatter | G2 | Cold scattering pure CO2 |
Notes. The paper references are Rocha & Pilling (2014) for model G2, and Rocha et al. (2017) for models D13a, D12a, and D2a. The mass ratio in the D13a and D12a models is 10/1/1/1, in the D2a model it is 10/1.
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