Rights statement: Accepted for publication in Journal of Geophysical Research: Space Physics. Copyright 2017 American Geophysical Union. Further reproduction or electronic distribution is not permitted
Accepted author manuscript, 4.09 MB, PDF document
Available under license: CC BY-NC: Creative Commons Attribution-NonCommercial 4.0 International License
Rights statement: ©2017. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
Final published version, 3.14 MB, PDF document
Available under license: CC BY: Creative Commons Attribution 4.0 International License
Final published version
Licence: CC BY: Creative Commons Attribution 4.0 International License
Research output: Contribution to Journal/Magazine › Journal article › peer-review
Research output: Contribution to Journal/Magazine › Journal article › peer-review
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TY - JOUR
T1 - An isolated, bright cusp aurora at Saturn
AU - Kinrade, Joe
AU - Badman, Sarah Victoria
AU - Bunce, E. J.
AU - Tao, C.
AU - Provan, G.
AU - Cowley, S. W. H.
AU - Grocott, Adrian
AU - Gray, Rebecca
AU - Grodent, D. C.
AU - Kimura, T.
AU - Nichols, J. D.
AU - Arridge, Christopher Stephen
AU - Radioti, Aikaterini
AU - Clarke, J. T.
AU - Crary, F. J.
AU - Pryor, W. R.
AU - Melin, Henrik
AU - Baines, Kevin H.
AU - Dougherty, Michele K.
N1 - ©2017. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
PY - 2017/6
Y1 - 2017/6
N2 - Saturn's dayside aurora display a number of morphological features poleward of the main emission region. We present an unusual morphology captured by the Hubble Space Telescope on 14 June 2014 (day 165), where, for two hours, Saturn's FUV aurora faded almost entirely, with the exception of a distinct emission spot at high latitude. The spot remained fixed in local time between 10-15 LT, and moved polewards to a minimum colatitude of ~4°. It was bright and persistent, displaying intensities of up to 49 kR over a lifetime of two hours. Interestingly the spot constituted the entirety of the northern auroral emission, with no emissions present at any other local time – including Saturn's characteristic dawn arc, the complete absence of which is rarely observed. Solar wind parameters from propagation models, together with a Cassini magnetopause crossing and solar wind encounter, indicate that Saturn's magnetosphere was likely to have been embedded in a rarefaction region, resulting in an expanded magnetosphere configuration during the interval. We infer that the spot was sustained by reconnection either poleward of the cusp, or at low latitudes under a strong component of interplanetary magnetic field transverse to the solar wind flow. The subsequent poleward motion could then arise from either reconfiguration of successive open field lines across the polar cap, or convection of newly opened field lines. We also consider the possible modulation of the feature by planetary period rotating current systems.
AB - Saturn's dayside aurora display a number of morphological features poleward of the main emission region. We present an unusual morphology captured by the Hubble Space Telescope on 14 June 2014 (day 165), where, for two hours, Saturn's FUV aurora faded almost entirely, with the exception of a distinct emission spot at high latitude. The spot remained fixed in local time between 10-15 LT, and moved polewards to a minimum colatitude of ~4°. It was bright and persistent, displaying intensities of up to 49 kR over a lifetime of two hours. Interestingly the spot constituted the entirety of the northern auroral emission, with no emissions present at any other local time – including Saturn's characteristic dawn arc, the complete absence of which is rarely observed. Solar wind parameters from propagation models, together with a Cassini magnetopause crossing and solar wind encounter, indicate that Saturn's magnetosphere was likely to have been embedded in a rarefaction region, resulting in an expanded magnetosphere configuration during the interval. We infer that the spot was sustained by reconnection either poleward of the cusp, or at low latitudes under a strong component of interplanetary magnetic field transverse to the solar wind flow. The subsequent poleward motion could then arise from either reconfiguration of successive open field lines across the polar cap, or convection of newly opened field lines. We also consider the possible modulation of the feature by planetary period rotating current systems.
U2 - 10.1002/2016JA023792
DO - 10.1002/2016JA023792
M3 - Journal article
VL - 122
SP - 6121
EP - 6138
JO - Journal of Geophysical Research: Space Physics
JF - Journal of Geophysical Research: Space Physics
SN - 2169-9402
IS - 6
ER -