TY - JOUR
T1 - Simultaneous Cassini VIMS and UVIS observations of Saturn's southern aurora
T2 - Comparing emissions from H, H2 and H3+ at a high spatial resolution
AU - Melin, H.
AU - Stallard, T.
AU - Miller, S.
AU - Gustin, J.
AU - Galand, M.
AU - Badman, S. V.
AU - Pryor, W. R.
AU - O'Donoghue, J.
AU - Brown, R. H.
AU - Baines, K. H.
PY - 2011/8/1
Y1 - 2011/8/1
N2 - Here, for the first time, temporally coincident and spatially overlapping Cassini VIMS and UVIS observations of Saturn's southern aurora are presented. Ultraviolet auroral H and H2 emissions from UVIS are compared to infrared H3+ emission from VIMS. The auroral emission is structured into three arcs-H, H2 and H3+ are morphologically identical in the bright main auroral oval (∼73°S), but there is an equatorward arc that is seen predominantly in H (∼70°S), and a poleward arc (∼74°S) that is seen mainly in H2 and H 3+. These observations indicate that, for the main auroral oval, UV emission is a good proxy for the infrared H3+ morphology (and vice versa), but for emission either poleward or equatorward this is no longer true. Hence, simultaneous UV/IR observations are crucial for completing the picture of how the atmosphere interacts with the magnetosphere.
AB - Here, for the first time, temporally coincident and spatially overlapping Cassini VIMS and UVIS observations of Saturn's southern aurora are presented. Ultraviolet auroral H and H2 emissions from UVIS are compared to infrared H3+ emission from VIMS. The auroral emission is structured into three arcs-H, H2 and H3+ are morphologically identical in the bright main auroral oval (∼73°S), but there is an equatorward arc that is seen predominantly in H (∼70°S), and a poleward arc (∼74°S) that is seen mainly in H2 and H 3+. These observations indicate that, for the main auroral oval, UV emission is a good proxy for the infrared H3+ morphology (and vice versa), but for emission either poleward or equatorward this is no longer true. Hence, simultaneous UV/IR observations are crucial for completing the picture of how the atmosphere interacts with the magnetosphere.
UR - http://www.scopus.com/inward/record.url?scp=80051749366&partnerID=8YFLogxK
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U2 - 10.1029/2011GL048457
DO - 10.1029/2011GL048457
M3 - Article
AN - SCOPUS:80051749366
SN - 0094-8276
VL - 38
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 15
M1 - L15203
ER -