This blog post is based on the papers “Evolution of the ion environment of comet 67P/Churyumov-Gerasimenko: Observations between 3.6 and 2.0 AU ” by H. Nilsson et al.; “Rosetta observations of solar wind interaction with the comet 67P/Churyumov-Gerasimenko” by T.
W. Broiles et al.; and “Solar Wind Sputtering of Dust on the Surface of 67P/Churyumov-Gerasimenko ” by Peter Wurz et al.,which have all been accepted for publication in Astronomy and Astrophysics, and “Dynamical features and spatial structures of the plasma interaction region of 67P/Churyumov–Gerasimenko and the solar wind” by C. Koenders et al, or which is published in Planetary and Space Science. Rosetta is making safe progress in one of its key investigations,which concerns the interaction between the comet and the solar wind. The solar wind is the constant stream of electrically charged particles that flows from the Sun, carrying its magnetic field out into the Solar System. Like all comets, or 67P/Churyumov–Gerasimenko must navigate this flow in its orbit around the Sun. It is the constant battle fought between the comet and the solar wind that helps to sculpt the comet’s ion tail. Rosetta’s instruments are monitoring the fine detail of this process. Using the Rosetta Plasma Consortium Ion Composition Analyzer,Hans Nilsson from the Swedish Institute of Space Physics and his colleagues have been studying the gradual evolution of the comet’s ion environment. They have seen that the number of water ions molecules of water that have been stripped of one electron – accelerated absent from the comet increased hugely as 67P/C-G moved between 3.6AU (approximately 538 million km) and 2.0AU (approximately 300 million km) from the Sun. Although the day-to-day acceleration is highly variable, the average 24-hour rate has increased by a factor of 10000 during the study, or which covered the period August 2014 to March 2015. The water […]
Source: esa.int