Solar Wind Protons Forming Partial Ring Distributions at Comet 67P

• Published in: Journal of geophysical research. Space physics 2023-02, Vol.128 (2), p.n/a
• Main Authors: Moeslinger, A., Wieser, G. Stenberg, Nilsson, H., Gunell, H., Williamson, H. N., LLera, K., Odelstad, E., Richter, I.
• Format: Article
• Language: English
• Subjects: 6025; Alpha particles; Alpha rays; Angular distribution; Comets; Deflection; Density; Energy distribution; Gyration; Interplanetary space; Ion composition; Ions; Protons; Rosetta mission; Solar wind; Solar wind protons; Spacecraft; Trajectories
• ISSN: 2169-9380; 2169-9402; 2169-9402
• DOI: 10.1029/2022JA031082

We present partial ring distributions of solar wind protons observed by the Rosetta spacecraft at comet 67P/Churyumov‐Gerasimenko. The formation of ring distributions is usually associated with high activity comets, where the spatial scales are larger than multiple ion gyroradii. Our observations are made at a low‐activity comet at a heliocentric distance of 2.8 AU on 19 April 2016, and the partial rings occur at a spatial scale comparable to the ion gyroradius. We use a new visualization method to simultaneously show the angular distribution of median energy and differential flux. A fitting procedure extracts the bulk speed of the solar wind protons, separated into components parallel and perpendicular to the gyration plane, as well as the gyration velocity. The results are compared with models and put into context of the global comet environment. We find that the formation mechanism of these partial rings of solar wind protons is entirely different from the well‐known partial rings of cometary pickup ions at high‐activity comets. A density enhancement layer of solar wind protons around the comet is a focal point for proton trajectories originating from different regions of the upstream solar wind. If the spacecraft location coincides with this density enhancement layer, the different trajectories are observed as an energy‐angle dispersion and manifest as partial rings in velocity space. Plain Language Summary Particles of solar origin, called the “solar wind,” flow straight from the Sun in interplanetary space. When this solar wind meets an obstacle, such as a planet, it gets deflected around it. At comet 67P/Churyumov‐Gerasimenko, visited by the Rosetta spacecraft from 2014 to 2016, our instrument Rosetta Plasma Consortium (RPC)‐Ion Composition Analyzer (ICA) measured the main constituents of this solar wind: protons and alpha particles. When the comet is far away from the Sun, the solar wind protons are usually observed coming from the sunward direction with only slight deflection and constant velocities. On 19 April 2016, the main case for our study, we measure solar wind protons arriving in a wide range of directions. The velocity of these protons depends on how much they have been deflected. This creates partial ring distributions, which we visualize and quantify using a method specifically developed for this purpose. We show that these partial rings are a rare observation of a spatially confined region where solar wind protons from different region