Vertical structure of the near-surface expanding ionosphere of comet 67P probed by Rosetta

K. Heritier 1 Pierre Henri 2 Xavier Vallières 2 M. Galand 1 E. Odelstad 3 A. I. Eriksson 4 F. L. Johansson 4 K. Altwegg 5 E. Behar 3 A. Beth 6 T. W. Broiles 7 J. L. Burch 7 C. M. Carr 8 E. Cupido 9 H. Nilsson 3 M. Rubin 5 E. Vigren 3
1 Imperial College London
2 LPC2E - Laboratoire de Physique et Chimie de l'Environnement et de l'Espace
3 IRF - Swedish Institute of Space Physics [Uppsala]
4 IRF - Swedish Institute of Space Physics [Kiruna]
5 Physikalisches Institut [Bern]
6 Department of Physics [London]
7 Space Science Division [San Antonio]
8 Space and Atmospheric Physics Group [London]
Blackett Laboratory
9 Blackett Laboratory
Abstract : The plasma environment has been measured for the first time near the surface of a comet. This unique data set has been acquired at 67P/Churyumov–Gerasimenko during ESA/Rosetta spacecraft's final descent on 2016 September 30. The heliocentric distance was 3.8 au and the comet was weakly outgassing. Electron density was continuously measured with Rosetta Plasma Consortium (RPC)–Mutual Impedance Probe (MIP) and RPC–LAngmuir Probe (LAP) during the descent from a cometocentric distance of 20 km down to the surface. Data set from both instruments have been cross-calibrated for redundancy and accuracy. To analyse this data set, we have developed a model driven by Rosetta Orbiter Spectrometer for Ion and Neutral Analysis–COmetary Pressure Sensor total neutral density. The two ionization sources considered are solar extreme ultraviolet radiation and energetic electrons. The latter are estimated from the RPC–Ion and Electron Sensor (IES) and corrected for the spacecraft potential probed by RPC–LAP. We have compared the results of the model to the electron densities measured by RPC–MIP and RPC–LAP at the location of the spacecraft. We find good agreement between observed and modelled electron densities. The energetic electrons have access to the surface of the nucleus and contribute as the main ionization source. As predicted, the measurements exhibit a peak in the ionospheric density close to the surface. The location and magnitude of the peak are estimated analytically. The measured ionospheric densities cannot be explained with a constant outflow velocity model. The use of a neutral model with an expanding outflow is critical to explain the plasma observations.
Keywords : plasmas methods: data analysis comets: individual: 67P Sun: UV radiation
Type de document :
Article dans une revue
Monthly Notices of the Royal Astronomical Society, Oxford University Press (OUP): Policy P - Oxford Open Option A, 2017, 469 (Suppl_2), pp.S118-S129. 〈10.1093/mnras/stx1459〉
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K. Heritier, Pierre Henri, Xavier Vallières, M. Galand, E. Odelstad, et al.. Vertical structure of the near-surface expanding ionosphere of comet 67P probed by Rosetta. Monthly Notices of the Royal Astronomical Society, Oxford University Press (OUP): Policy P - Oxford Open Option A, 2017, 469 (Suppl_2), pp.S118-S129. 〈10.1093/mnras/stx1459〉. 〈insu-01670766〉

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