Abstract

Context.During its two-year mission at comet 67P, Rosetta nearly continuously monitored the inner coma plasma environment for gas production rates varying over three orders of magnitude, at distances to the nucleus ranging from a few to a few hundred kilometres. To achieve the best possible measurements, cross-calibration of the plasma instruments is needed.Aims.Our goal is to provide a consistent plasma density dataset for the full mission, while in the process providing a statistical characterisation of the plasma in the inner coma and its evolution.Methods.We constructed physical models for two different methods to cross-calibrate the spacecraft potential and the ion current as measured by the Rosetta Langmuir probes (LAP) to the electron density as measured by the Mutual Impedance Probe (MIP). We also described the methods used to estimate spacecraft potential, and validated the results with the Ion Composition Analyser (ICA).Results.We retrieve a continuous plasma density dataset for the entire cometary mission with a much improved dynamical range compared to any plasma instrument alone and, at times, improve the temporal resolution from 0.24−0.74 Hz to 57.8 Hz. The physical model also yields, at a three-hour time resolution, ion flow speeds and a proxy for the solar EUV flux from the photoemission from the Langmuir probes.Conclusions.We report on two independent mission-wide estimates of the ion flow speed that are consistent with the bulk H2O+ion velocities as measured by the ICA. We find the ion flow to consistently be much faster than the neutral gas over the entire mission, lending further evidence that the ions are collisionally decoupled from the neutrals in the coma. Measurements of ion speeds from Rosetta are therefore not consistent with the assumptions made in previously published plasma density models of the comet 67P’s ionosphere at the start and end of the mission. Also, the measured EUV flux is perfectly consistent with independently derived values previously published from LAP and lends support for the conclusions drawn regarding an attenuation of solar EUV from a distant nanograin dust population, when the comet activity was high. The new density dataset is consistent with the existing MIP density dataset, but it facilitates plasma analysis on much shorter timescales, and it also covers long time periods where densities were too low to be measured by MIP.

Highlights

  • The European Space Agency’s comet chaser Rosetta studied the comet 67P/Churyumov-Gerasimenko in unprecedented detail for more than two years from August 2014 to September 2016 (Taylor et al 2017)

  • In what amounted to a halfrevolution around the sun, the scientific package dedicated to the plasma environment, the Rosetta Plasma Consortium (RPC, Carr et al 2007), studied the comet as it evolved through different activity levels including perihelion at 1.24 AU and the dwindling activity at the end of the mission at 3.83 AU

  • After a brief description of the instruments used in this study in Sect. 2, we describe the spacecraft potential as measured by Langmuir probes (LAP) and how we can verify that measurement using the attracted ions observed by the Ion Composition Analyser (ICA) in Sect

Read more

Summary

Introduction

The European Space Agency’s comet chaser Rosetta studied the comet 67P/Churyumov-Gerasimenko in unprecedented detail for more than two years from August 2014 to September 2016 (Taylor et al 2017). Cometary electrons are significantly repelled from the Langmuir probe (Eriksson et al 2017; Johansson et al 2020), and positive ions are perturbed (Bergman et al 2020a,b). As such, this poses significant challenges to the RPC’s ability to characterise the low-energy cometary plasma that dominates the comet environment (Edberg et al 2015; Odelstad et al 2018; Gilet et al 2019; Wattieaux et al 2020), but this can be Article published by EDP Sciences

Objectives
Methods
Results
Discussion
Conclusion
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.