Issue |
A&A
Volume 618, October 2018
|
|
---|---|---|
Article Number | A114 | |
Number of page(s) | 10 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/201833300 | |
Published online | 17 October 2018 |
First observations of magnetic holes deep within the coma of a comet
1
Space Research Institute, Austrian Academy of Sciences,
Schmiedlstrasse 6,
8042 Graz,
Austria
e-mail: ferdinand.plaschke@oeaw.ac.at
2
Department of Space and Plasma Physics, School of Electrical Engineering and Computer Science, Royal Institute of Technology,
Stockholm,
Sweden
3
Institute of Geophysics and Extraterrestrial Physics, Braunschweig Institute of Technology,
Braunschweig,
Germany
4
Swedish Institute of Space Physics,
Uppsala,
Sweden
5
Swedish Institute of Space Physics,
Kiruna,
Sweden
6
Southwest Research Institute,
San Antonio,
USA
Received:
25
April
2018
Accepted:
5
July
2018
The Rosetta spacecraft of the European Space Agency made ground-breaking observations of comet 67P/Churyumov-Gerasimenko and of its cometary environment. We search for magnetic holes in that environment, i.e., significant depressions in the magnetic field strength, measured by the Rosetta fluxgate Magnetometer (MAG) in April and May 2015. In that time frame of two months, we identified 23 magnetic holes. The cometary activity was intermediate and increasing because Rosetta was on the inbound leg toward the Sun. While in April solar wind protons were still observed by Rosetta near the comet, in May these protons were already mostly replaced by heavy cometary ions. Magnetic holes have frequently been observed in the solar wind. We find, for the first time, that magnetic holes exist in the cometary environment even when solar wind protons are almost absent. Some of the properties of the magnetic holes are comparable to those of solar wind holes; they are associated with density enhancements, sometimes associated with co-located current sheets and fast solar wind streams, and are of similar scales. However, particularly in May, the magnetic holes near the comet appear to be more processed, featuring shifted density enhancements and, sometimes, bipolar signatures in magnetic field strength rather than simple depressions. The magnetic holes are of global size with respect to the coma. However, at the comet, they are compressed owing to magnetic field pile-up and draping so that they change in shape. There, the magnetic holes become of comparable size to heavy cometary ion gyroradii, potentially enabling kinetic interactions.
Key words: plasmas / magnetohydrodynamics (MHD) / instabilities / comets: general / interplanetary medium
© ESO 2018
Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.