EGU21-7657, updated on 04 Mar 2021
https://doi.org/10.5194/egusphere-egu21-7657
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Jupiter's X-ray aurora during a mass injection and Io mass loading events observed by XMM-Newton, Hubble, and Hisaki

Affelia Wibisono1,2, Graziella Branduardi-Raymont1,2, Will Dunn1,2, Tomoki Kimura3, Andrew Coates1,2, Denis Grodent4, Zhonghua Yao5, Hajime Kita6, Pedro Rodriguez7, Randy Gladstone8, Bertrand Bonfond4, and Richard Haythornthwaite1,2
Affelia Wibisono et al.
  • 1University College London, Mullard Space Science Laboratory, Space and Climate Physics, Dorking, United Kingdom of Great Britain – England, Scotland, Wales (affelia.wibisono.18@ucl.ac.uk)
  • 2The Centre for Planetary Science at UCL/Birkbeck, Gower Street, London, UK
  • 3Frontier Research Institute for Interdisciplinary Sciences Tohoku University, Japan
  • 4Laboratoire de Physique Atmospherique et Planetaire, Universite de Liege, Liege, Belgium
  • 5Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
  • 6Department of Information and Communication Engineering, Tohoku Institute of Technology, Japan
  • 7European Space Astronomy Centre, Madrid, Spain
  • 8Southwest Research Institute, San Antonio, Texas, USA

Voyager 1 detected the first extra-terrestrial UV auroral emissions when it explored the Jupiter system in 1979 while the planet’s X-ray aurora was discovered later that year by the Einstein Observatory. Electrons are accelerated into Jupiter’s atmosphere near the poles and excite native molecular and atomic hydrogen. These then release UV photons after returning to the ground state. The same population of precipitating electrons can also emit high energy (>2 keV) X-ray photons by bremsstrahlung to produce Jupiter’s hard X-ray aurora. At higher latitudes and within the oval of UV and hard X-ray emissions is where the more diffuse UV and low energy (<2 keV) soft X-ray aurorae are found.  Charge exchange processes between precipitating ions and neutrals in the gas giant planet’s atmosphere are responsible for the soft X-ray emissions.

Simultaneous observations of Jupiter’s UV and X-ray aurorae were carried out by the Hubble Space Telescope (HST), Hisaki satellite and XMM-Newton in September 2019 to support Juno’s 22nd perijove. Images of the northern far UV aurora by HST showed internally driven dawn storms and injection events occurring at least twice during the observation period. These features are thought to be caused by magnetic reconnection happening in the middle magnetosphere. This subsequently leads to the dipolarization of the field lines which injects hot magnetospheric plasma from the middle to the inner magnetosphere. Hisaki saw an impulsive brightening in the Io plasma torus on the day of the second event showing that there was indeed a large-scale injection that penetrated the central torus in the inner magnetosphere. At this time, the northern aurora brightened in both extreme UV and hard X-ray, which suggests that there was an increase in electron precipitation.  There was no response from the soft X-ray aurora, and no quasi-periodic pulsations, often observed in the auroral emissions, were detected during either of the events. X-ray spectral analysis reveals that the precipitating ions were iogenic. We conclude that we have witnessed two cases of mass injection in the Jovian inner magnetosphere due to Io mass loading events.

How to cite: Wibisono, A., Branduardi-Raymont, G., Dunn, W., Kimura, T., Coates, A., Grodent, D., Yao, Z., Kita, H., Rodriguez, P., Gladstone, R., Bonfond, B., and Haythornthwaite, R.: Jupiter's X-ray aurora during a mass injection and Io mass loading events observed by XMM-Newton, Hubble, and Hisaki, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-7657, https://doi.org/10.5194/egusphere-egu21-7657, 2021.

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