Introduction
Comets as Natural Laboratories for Space Plasma MeasurementsThe neutral gas coma of an active comet is subject to ionization by solar EUV radiation (as well as charge exchange and electron impact reactions with the solar wind and high-energy electrons, see e.g., Cravens, 1991). It thus provides an extended source of newly ionized plasma to the surrounding interplanetary medium, otherwise dominated by the solar wind (hereafter SW). The resulting interaction between SW and cometary plasma (e.g., Neugebauer, 1990) gives rise to an abundance of plasma instabilities, waves and turbulent phenomena (Tsurutani, 1991). The cometary plasma environment therefore provides an excellent setting for studying such processes, which often play important roles in the physics and dynamics of plasmas. For example, they can heat or cool plasma populations, produce supra-thermal electrons, reduce plasma anisotropies and gradients, couple different plasma species to each other, and provide anomalous resistivity.
The Rosetta MissionThe European Space Agency's Rosetta mission (Glassmeier, Boehnhardt, et al., 2007;Taylor et al., 2017) brought a spacecraft to the comet 67P/Churyumov-Gerasimenko (hereafter 67P), following it in its orbit around the Sun from August 2014 (at 3.6 au from the Sun) through perihelion in August 2015 (at 1.24 au) until the end of September 2016 (3.8 au). The instruments of the Rosetta Plasma Consortium (RPC;Carr et al., 2007) thus got an unprecedented long-term view of the near-nucleus cometary plasma environment of an intermediately active comet, for which the production rate varied between ∼4 × 10 25 s −1 and ∼3.5 × 10 28 s −1 during the mission (Hansen et al., 2016;Heritier et al., 2017). The spacecraft mostly stayed in close to terminator orbit within about 400 km of the nucleus (with the exception of two brief (≲1 month) sunward and tailward excursions to beyond ∼1,000 km).