From CO2- to H2O-dominated atmospheres and back - How mixed outgassing changes the volatile distribution in magma oceans around M dwarf stars

Open Access

Table D.1

Run times of TRAPPIST-1 g simulations with initial CO₂ mass equal to the initial H₂O mass.

Initial water mass [TO]	1	2	100
RT atmosphere model

ϵ = 10^–1	6 min 11 s	6 min 4 s	6 min 1 s
ϵ = 10^–2	10 min 22 s	11 min 25 s	11 min 15 s
ϵ = 10^–3	27 min 41 s	22 min 54 s	22 min 40 s

Corrected gray atmosphere model

ϵ = 10^–1	0 min 40 s	0 min 41 s	0 min 41 s
ϵ = 10^–2	0 min 45 s	0 min 48 s	0 min 47 s
ϵ = 10^–3	1 min 3 s	1 min 2 s	1 min 2

On a state-of-the-art multicore machine with different numerical accuracies ϵ.

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