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Evidence of sub-surface energy storage in comet 67P from the outburst of 2016 July 03

AutorAgarwal, J.; Della Corte, V.; Feldman, P.D.; Geiger, B.; Merouane, S.; Bertini, I.; Bodewits, D.; Fornasier, S.; Grün, E.; Hasselmann, P.; Hilchenbach, M.; Höfner, S.; Ivanovski, S.; Kolokolova, L.; Pajola, M.; Rotundi, A.; Sierks, H.; Steffl, A.J.; Thomas, N.; A'Hearn, M.F.; Barbieri, C.; Barucci, M.A.; Bertaux, J.L.; Boudreault, S.; Cremonese, G.; Da Deppo, V.; Davidsson, B.; Debei, S.; De Cecco, M.; Deller, J.F.; Feaga, L.M.; Fischer, H.; Fulle, M.; Gicquel, A.; Groussin, O.; Güttler, C.; Gutiérrez, Pedro J. ; Hofmann, M.; Hornung, K.; Hviid, S.F.; Ip, W.H.; Jorda, L.; Keller, H.U.; Kissel, J.; Knollenberg, J.; Koch, A.; Koschny, D.; Kramm, J.R.; Kührt, E.; Küppers, M.; Langevin, Y.; Lara, Luisa María ; López-Moreno, José Juan ; Rodrigo Montero, Rafael
Palabras claveScattering
Solid state: volatile
Solid state: refractory
Acceleration of particles
Comets: general
Comets: individual: 67P/Churyumov-Gerasimenko
Fecha de publicación2017
EditorOxford University Press
CitaciónMonthly Notices of the Royal Astronomical Society 469: S606- S625 (2017)
ResumenOn 2016 July 03, several instruments onboard ESA's Rosetta spacecraft detected signs of an outburst event on comet 67P, at a heliocentric distance of 3.32 au from the Sun, outbound from perihelion. We here report on the inferred properties of the ejected dust and the surface change at the site of the outburst. The activity coincided with the local sunrise and continued over a time interval of 14-68 min. It left a 10-m-sized icy patch on the surface. The ejected material comprised refractory grains of several hundred microns in size, and sub-micron-sized water ice grains. The high dust mass production rate is incompatible with the free sublimation of crystalline water ice under solar illumination as the only acceleration process. Additional energy stored near the surface must have increased the gas density. We suggest a pressurized sub-surface gas reservoir, or the crystallization of amorphous water ice as possible causes.© 2015 The Authors.
URIhttp://hdl.handle.net/10261/167581
Identificadoresdoi: 10.1093/mnras/stx2386
issn: 1365-2966
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