Fig. 9

Mixing ratio profiles of H2O, CO, and CO2 obtained when a production rate due to ice grain ablation for every species with integrated rates of 6.0 × 104, 2.45 × 104 and 4.5 × 103 cm−2 s−1 is taken into account. An additional source of cometary CO is considered as well, the impactor size is D = 2 km, and the evolution time needed to match the Herschel observations is 639 yr. The red dashed line refers to the carbon monoxide profile resulting from the simulation of case 2 (see Table 4).
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