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Io's Atmospheric Response to Eclipse: UV Aurorae Observations

机译:艾奥对日食的大气响应:紫外线极光观测

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The New Horizons (NH) spacecraft observed Io's aurora in eclipse on four occasions during spring 2007. NH Alice ultraviolet spectroscopy and concurrent Hubble Space Telescope ultraviolet imaging in eclipse investigate the relative contribution of volcanoes to Io's atmosphere and its interaction with Jupiter's magnetosphere. Auroral brightness and morphology variations after eclipse ingress and egress reveal changes in the relative contribution of sublimation and volcanic sources to the atmosphere. Brightnesses viewed at different geometries are best explained by a dramatic difference between the dayside and nightside atmospheric density. Far-ultraviolet aurora morphology reveals the influence of plumes on Io's electrodynamic interaction with Jupiter's magnetosphere. Comparisons to detailed simulations of Io's aurora indicate that volcanoes supply 1 to 3% of the dayside atmosphere.
机译:新视野号航天器在2007年春季四次在日食中观测到了艾欧的极光。日食中的NH爱丽丝紫外线光谱和哈勃太空望远镜紫外线成像研究了火山对艾奥大气的相对贡献及其与木星磁层的相互作用。日食进出后的极光亮度和形态变化揭示了升华和火山源对大气的相对贡献的变化。在白天和夜晚的大气密度之间存在巨大差异,可以最好地解释在不同几何形状下查看的亮度。极紫外极光形态揭示了羽流对Io与木星磁层的电动力相互作用的影响。与艾奥极光的详细模拟进行的比较表明,火山提供了白天大气的1-3%。

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