“…Thanks to the continuous monitoring of the target by the orbiter, it was realized that there is much variability in the outgassing of ices hidden underneath the surface, which has to do with seasonal and diurnal variations as probed with Rosetta Orbiter Spectrometer for Ion and Neutral Analysis (ROSINA), Visible and Infrared Thermal Imaging Spectrometer (VIRTIS), Microwave Instrument for the Rosetta Orbiter (MIRO) and Optical, Spectroscopic, and Infrared Remote Imaging System (OSIRIS) instruments aboard Rosetta (e.g., De Sanctis et al 2015;Lee et al 2015;Bockelée-Morvan et al 2015b;Biver et al 2015;Luspay-Kuti et al 2015;Hässig et al 2015;Filacchione et al 2016a,b;Fornasier et al 2016;Hansen et al 2016;Bockelée-Morvan et al 2016;Barucci et al 2016;Migliorini et al 2016;Gasc et al 2017;Marshall et al 2017;Filacchione et al 2019). The bi-lobate geometry of the nucleus and the associated self-shielding, its changing rotational period, backfall of granular material, short-lived outbursts, active sinkhole pits and orbital trajectory change the irradiance of its surface during a single apparition (Keller et al 2015;Vincent et al 2015Vincent et al , 2016Feldman et al 2016;Keller et al 2017;Kramer et al 2018), but also in the long term upon repeated approaches to the Sun. Nevertheless, it is possible to extract bulk abundances of the interior ices upon careful data analysis (e.g., Calmonte et al 2016) and to peek at them on special occasions such as cliff collapses (Pajola et al 2017).…”