Please use this identifier to cite or link to this item: http://hdl.handle.net/2381/29290
Title: Cassini nightside observations of the oscillatory motion of Saturn's northern auroral oval
Authors: Bunce, Emma J.
Grodent, D. C.
Jinks, S. L.
Andrews, D. J.
Badman, S. V.
Coates, A. J.
Cowley, S. W. H.
Dougherty, M. K.
Kurth, W. S.
Mitchell, D. G.
Provan, G.
First Published: 16-May-2014
Publisher: American Geophysical Union
Citation: Journal of Geophysical Research : Space Physics, 2014, 119 (5), pp. 3528-3543
Abstract: In recent years we have benefitted greatly from the first in-orbit multi-wavelength images of Saturn's polar atmosphere from the Cassini spacecraft. Specifically, images obtained from the Cassini UltraViolet Imaging Spectrograph (UVIS) provide an excellent view of the planet's auroral emissions, which in turn give an account of the large-scale magnetosphere-ionosphere coupling and dynamics within the system. However, obtaining near-simultaneous views of the auroral regions with in situ measurements of magnetic field and plasma populations at high latitudes is more difficult to routinely achieve. Here we present an unusual case, during Revolution 99 in January 2009, where UVIS observes the entire northern UV auroral oval during a 2 h interval while Cassini traverses the magnetic flux tubes connecting to the auroral regions near 21 LT, sampling the related magnetic field, particle, and radio and plasma wave signatures. The motion of the auroral oval evident from the UVIS images requires a careful interpretation of the associated latitudinally “oscillating” magnetic field and auroral field-aligned current signatures, whereas previous interpretations have assumed a static current system. Concurrent observations of the auroral hiss (typically generated in regions of downward directed field-aligned current) support this revised interpretation of an oscillating current system. The nature of the motion of the auroral oval evident in the UVIS image sequence, and the simultaneous measured motion of the field-aligned currents (and related plasma boundary) in this interval, is shown to be related to the northern hemisphere magnetosphere oscillation phase. This is in agreement with previous observations of the auroral oval oscillatory motion.
DOI Link: 10.1002/2013JA019527
eISSN: 2169-9380
Links: http://onlinelibrary.wiley.com/doi/10.1002/2013JA019527/abstract;jsessionid=E2DE2ECB779C586848BA84FE9ECD6A9C.f01t04
http://hdl.handle.net/2381/29290
Version: Publisher Version
Status: Peer-reviewed
Type: Journal Article
Rights: Copyright © the authors, 2014. This is an open-access article distributed under the terms of the Creative Commons Attribution License ( http://creativecommons.org/licenses/by/3.0/ ), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Appears in Collections:Published Articles, Dept. of Physics and Astronomy

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