TY - JOUR
T1 - Variability of Jupiter's IR H3+ aurorae during Juno approach
AU - Moore, L.
AU - O'Donoghue, J.
AU - Melin, H.
AU - Stallard, T.
AU - Tao, C.
AU - Zieger, B.
AU - Clarke, J.
AU - Vogt, M. F.
AU - Bhakyapaibul, T.
AU - Opher, M.
AU - Tóth, G.
AU - Connerney, J. E. P.
AU - Levin, S.
AU - Bolton, S.
PY - 2017/5/28
Y1 - 2017/5/28
N2 - We present ground-based observations of Jupiter's H3+ aurorae over four nights in April 2016 while the Juno spacecraft was monitoring the upstream interplanetary magnetic field. High-precision maps of auroral H3+ densities, temperatures, and radiances reveal significant variabilities in those parameters, with regions of enhanced density and emission accompanied by reduced temperature. Juno magnetometer data, combined with solar wind propagation models, suggest that a shock may have impacted Jupiter in the days preceding the observation interval but that the solar wind was quiescent thereafter. Auroral H3+ temperatures reveal a downward temporal trend, consistent with a slowly cooling upper atmosphere, such as might follow a period of shock recovery. The brightest H3+ emissions are from the end of the period, 23 April. A lack of definitive signatures in the upstream interplanetary magnetic field lends supporting evidence to the possibility that this brightening event may have been driven by internal magnetospheric processes.
AB - We present ground-based observations of Jupiter's H3+ aurorae over four nights in April 2016 while the Juno spacecraft was monitoring the upstream interplanetary magnetic field. High-precision maps of auroral H3+ densities, temperatures, and radiances reveal significant variabilities in those parameters, with regions of enhanced density and emission accompanied by reduced temperature. Juno magnetometer data, combined with solar wind propagation models, suggest that a shock may have impacted Jupiter in the days preceding the observation interval but that the solar wind was quiescent thereafter. Auroral H3+ temperatures reveal a downward temporal trend, consistent with a slowly cooling upper atmosphere, such as might follow a period of shock recovery. The brightest H3+ emissions are from the end of the period, 23 April. A lack of definitive signatures in the upstream interplanetary magnetic field lends supporting evidence to the possibility that this brightening event may have been driven by internal magnetospheric processes.
UR - https://www.scopus.com/pages/publications/85019696788
U2 - 10.1002/2017GL073156
DO - 10.1002/2017GL073156
M3 - Article
SN - 0094-8276
VL - 44
SP - 4513
EP - 4522
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 10
ER -