A&A 616, A21 (2018) Astronomy https://doi.org/10.1051/0004-6361/201832842 & c ESO 2018 Astrophysics The root of a comet tail: Rosetta ion observations at comet 67P/Churyumov–Gerasimenko E. Behar1,2, H. Nilsson1,2, P. Henri5, L. Berciˇ cˇ1,2, G. Nicolaou1,4, G. Stenberg Wieser1, M. Wieser1, B. Tabone7, M. Saillenfest6, and C. Goetz3 1 Swedish Institute of Space Physics, Kiruna, Sweden e-mail:
[email protected] 2 Luleå University of Technology, Department of Computer Science, Electrical and Space Engineering, Kiruna, Sweden 3 Technische Universität Braunschweig Institute for Geophysics and Extraterrestrial Physics, Mendelssohnstraße 3, 38106 Braunschweig, Germany 4 Mullard Space Science Laboratory, University College London, Dorking, UK 5 LPC2E, CNRS, Orléans, 45071, France 6 IMCCE, Observatoire de Paris, PSL Research University, CNRS, Sorbonne Université, UPMC Univ. Paris 06, LAL, Université de Lille, 75014 Paris, France 7 LERMA, Observatoire de Paris, PSL Research University, CNRS, Sorbonne Université, UPMC Univ. Paris 06, 75014 Paris, France Received 16 February 2018 / Accepted 19 April 2018 ABSTRACT Context. The first 1000 km of the ion tail of comet 67P/Churyumov–Gerasimenko were explored by the European Rosetta spacecraft, 2.7 au away from the Sun. Aims. We characterised the dynamics of both the solar wind and the cometary ions on the night-side of the comet’s atmosphere. Methods. We analysed in situ ion and magnetic field measurements and compared the data to a semi-analytical model. Results. The cometary ions are observed flowing close to radially away from the nucleus during the entire excursion. The solar wind is deflected by its interaction with the new-born cometary ions.