Redistribution of particles across the nucleus of comet 67P/Churyumov-Gerasimenko
By Nicolas Gonzalez Thomas, B. Davidsson, M. El-Maarry, S. Fornasier, L. Giacomini, A. Gracia-Berná, S. Hviid, W. Ip, Laurent Jorda, H. U. Keller and 45 more. 2015
153 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Nuclear and High Energy Physics
View Paper: https://www.semanticscholar.org/paper/c94f11b19ab110ece9b375e426bfc0928f1f42ea
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In Astronomy and Astrophysics
- Jean-Loup Bertaux
- M. Hässig
- G. Kovacs
- Stefano Mottola
- Nicolas Gonzalez Thomas
- E. Dishoeck
- M. Rubin
- Tamas I. Gombosi
In Nuclear and High Energy Physics
Citations in the corpus
- Insolation, erosion, and morphology of comet 67P/Churyumov-Gerasimenko (2015, background): “The surface of the neck area (called Hapi, see Thomas et al. 2015b; and El-Maarry et al. 2015, for region designations) is rather smooth and is slightly blue compared to the reddish overall spectrum (Capaccioni et al. 2015; Fornasier et al. 2015).”
- Elemental and molecular abundances in comet 67P/Churyumov-Gerasimenko (2019, background): “D/I ratios inside the nucleus versus in the coma are still a matter of debate, fuelled by the redisposition of material at 67P/C-G (Rubin et al. 2014; Thomas et al. 2015).”
- Shape model, reference system definition, and cartographic mapping standards for comet 67P/Churyumov-Gerasimenko Stereo-photogrammetric analysis of Rosetta/OSIRIS image data (2015, methodology): “7) at 157.82◦/71.99◦/1099 m. Region names are defined in Sierks et al. (2015) and Thomas et al. (2015b).”
- EVOLUTION OF THE DUST SIZE DISTRIBUTION OF COMET 67P/CHURYUMOV–GERASIMENKO FROM 2.2 au TO PERIHELION (2016, background): “Dust release and fallback, also defined as aeolian transfer of dust across the nucleus surface (Thomas et al. 2015), are time-dependent because they depend on the local rate of gas loss from the nucleus surface.”
- Sulphur-bearing species in the coma of comet 67P/Churyumov–Gerasimenko (2016, background): “MNRAS 462, S253–S273 (2016) D ow nloaded from https://academ ic.oup.com /m nras/article-abstract/462/Suppl_1/S253/2633389 by guest on 16 M arch 2020 transport of water ice grains during the perihelion passage to the dark side of the nucleus as observed earlier in the mission by the camera OSIRIS (Th”
- The Physics of Sediment Transport Initiation, Cessation, and Entrainment Across Aeolian and Fluvial Environments (2020, background): “Likewise, sublimation of subsurface ice in cold environments (the so-called solid-state greenhouse effect [Kaufmann et al., 2006]) can generate airborne particles of carbon dioxide, methane, and nitrogen ice [Hansen et al., 1990; Thomas et al., 2015; Jia et al., 2017; Telfer et al., 2018].”
- The primordial nucleus of comet 67P/Churyumov-Gerasimenko (2015, methodology): “Abydos consists of consolidated terrain (Thomas et al. 2015b) with S c ≈ 2 MPa according to Philae/MUPUS-PEN (Spohn et al. 2015).”