posted on 2018-05-25, 15:24authored byDenis 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
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