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Detection of Callisto's oxygen atmosphere with the Hubble Space Telescope

机译:哈勃太空望远镜探测卡利斯托的氧气气氛

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We report the result of a search for evidence of an O-2-dominated atmosphere on Callisto, using the high far-ultraviolet sensitivity of the Hubble Space Telescope Cosmic Origins Spectrograph (COS). Observations of Callisto's leading/Jupiter-facing hemisphere show, for the first time, variable-strength atomic oxygen (O I) emissions with brightness up to 4.7 +/- 0.7 Rayleighs for the O I 1304 A triplet and 1.9 +/- 0.4 Rayleighs for the O I 1356 angstrom doublet, averaged over the 2.5 arcsec. diameter COS aperture. Because the observations were made in Earth's shadow, and are brighter than expected emission from nighttime geocoronal airglow or other plausible sources, we are confident that they originate from Callisto or its immediate vicinity. In addition, COS's limited (similar to 1 arcsec) spatial resolution implies a 2 sigma detection of excess 1356 A emission concentrated on the disk of Callisto itself, with brightness 3.2 +/- 1.6 Rayleighs. The (O I 1356 angstrom)/(O I 1304 angstrom) emission ratio from Callisto's disk favors dissociative excitation of O-2, suggesting that O-2 is the dominant atmospheric component rather than other possible oxygen-bearing alternatives. Photoelectrons, rather than magnetospheric electrons, are the most likely source of the dissociative excitation. This detection yields an O-2 column density of similar to 4 x 10(15) cm(-2) on the leading/Jupiter facing hemisphere, which implies that Callisto's atmosphere is collisional and is the fourth-densest satellite atmosphere in the Solar System, in addition to being the second-densest O-2-rich collisional atmosphere in the Solar System, after Earth. Longitudinal variations in published densities of ionospheric electrons suggest that O-2 densities in Callisto's trailing hemisphere, which we did not observe, may be an order of magnitude greater. The aperture-filling emissions imply that there is also an extended corona of predominantly O I 1304 angstrom emission around Callisto, with observed strength of 1-4 Rayleighs, likely due to solar resonance scattering from sputtered atomic O, with a density of up to 10(4) cm(-3) at the exobase. (C) 2015 Elsevier Inc. All rights reserved.
机译:我们报告了使用哈勃太空望远镜宇宙起源光谱仪(COS)的高远紫外线敏感性在Callisto上寻找O-2为主的大气的证据的结果。卡里斯托(Callisto)面对木星前半球的观测首次显示出可变强度原子氧(OI)排放,OI 1304 A三重态的亮度高达4.7 +/- 0.7瑞利,而OI 1304 A三重态的亮度高达1.9 +/- 0.4瑞利。 OI 1356埃双峰,平均2.5弧秒。直径COS孔径。由于观测是在地球的阴影下进行的,并且比预期的夜间地球冠状气辉或其他合理来源的发射要明亮,因此我们有信心它们来自Callisto或其附近地区。此外,COS有限的空间分辨率(类似于1 arcsec)意味着对2356多余的1356 A辐射进行了检测,该辐射集中在Callisto本身的磁盘上,亮度为3.2 +/- 1.6瑞利。 Callisto盘的(O 1356埃)/(O 1304埃)发射比率有利于O-2的解离激发,这表明O-2是主要的大气成分,而不是其他可能的含氧替代物。光电子而不是磁层电子是最可能的解离激发源。此检测在面对前半球/木星的半球上产生的O-2列密度类似于4 x 10(15)cm(-2),这意味着Callisto的大气层是碰撞的,并且是太阳系中第四密度最大的卫星大气层。 ,它是继地球之后太阳系中第二密度最强的O-2碰撞大气。电离层电子的已发布密度的纵向变化表明,我们未观察到的卡利斯托后半球的O-2密度可能要大一个数量级。充满孔的发射表明,在Callisto周围还存在一个主要为OI 1304埃发射的延长电晕,观察到的强度为1-4瑞利,很可能是由于溅射原子O产生的太阳共振散射,其密度高达10( 4)cm(-3)在外基部。 (C)2015 Elsevier Inc.保留所有权利。

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