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Jupiter's Aurora Observed With HST During Juno Orbits 3 to 7

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posted on 2018-05-25, 15:24 authored by Denis Grodent, B. Bonfond, Z. Yao, J.‐C. Gérard, A. Radioti, M. Dumont, B. Palmaerts, A. Adriani, S. V. Badman, E. J. Bunce, J. T. Clarke, J. E. P. Connerney, G. R. Gladstone, T. Greathouse, T. Kimura, W. S. Kurth, B. H. Mauk, D. J. Mccomas, J. D. Nichols, G. S. Orton, L. Roth, J. Saur, P. Valek
A large set of observations of Jupiter's ultraviolet aurora was collected with the Hubble Space Telescope concurrently with the NASA-Juno mission, during an eight-month period, from 30 November 2016 to 18 July 2017. These Hubble observations cover Juno orbits 3 to 7 during which Juno in situ and remote sensing instruments, as well as other observatories, obtained a wealth of unprecedented information on Jupiter's magnetosphere and the connection with its auroral ionosphere. Jupiter's ultraviolet aurora is known to vary rapidly, with timescales ranging from seconds to one Jovian rotation. The main objective of the present study is to provide a simplified description of the global ultraviolet auroral morphology that can be used for comparison with other quantities, such as those obtained with Juno. This represents an entirely new approach from which logical connections between different morphologies may be inferred. For that purpose, we define three auroral subregions in which we evaluate the auroral emitted power as a function of time. In parallel, we define six auroral morphology families that allow us to quantify the variations of the spatial distribution of the auroral emission. These variations are associated with changes in the state of the Jovian magnetosphere, possibly influenced by Io and the Io plasma torus and by the conditions prevailing in the upstream interplanetary medium. This study shows that the auroral morphology evolved differently during the five ~2 week periods bracketing the times of Juno perijove (PJ03 to PJ07), suggesting that during these periods, the Jovian magnetosphere adopted various states.

Funding

B. B., D. G., Z. Y., B. P., and J. C. G. are supported by the PRODEX program managed by ESA in collaboration with the Belgian Federal Science Policy Office. A. R. was funded by the Fund for Scientific Research (F.R.S-FNRS). Z. Y. is funded by a Marie Curie COFUND postdoctoral fellowship. J. D. N. was supported by STFC grant ST/K001000/1. G. S. O. was supported by funds from the National Aeronautics and Space Administration distributed to the Jet Propulsion Laboratory, California Institute of Technology. The research at the University of Iowa was supported by NASA through contract 699041X with Southwest Research Institute. This research is based on observations with the NASA/ESA Hubble Space Telescope (program HST GO-14634), obtained at the Space Telescope Science Institute (STScI), which is operated by AURA for NASA. All data are publicly available at STScI. Solar wind parameters were propagated with the AMDA science analysis system provided by the Centre de Données de la Physique des Plasmas (CDPP) supported by CNRS, CNES, Observatoire de Paris, and Université Paul Sabatier, Toulouse. D. G. wishes to thank William Januszewski and John Debes, at STScI, for their invaluable help in programming the HST observations.

History

Citation

Journal of Geophysical Research: Space Physics, 2018,123

Author affiliation

/Organisation/COLLEGE OF SCIENCE AND ENGINEERING/Department of Physics and Astronomy

Version

  • VoR (Version of Record)

Published in

Journal of Geophysical Research: Space Physics

Publisher

American Geophysical Union (AGU), Wiley

issn

2169-9380

eissn

2169-9402

Acceptance date

2018-03-09

Copyright date

2018

Available date

2018-09-12

Publisher version

https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1002/2017JA025046

Notes

The file associated with this record is under embargo until 6 months after publication, in accordance with the publisher's self-archiving policy. The full text may be available through the publisher links provided above.

Language

en

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