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Morphology of the ultraviolet Io footprint emission and its control by Io's location

机译:形态学的紫外线Io足迹排放及其控制输入输出的位置

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A total of 74 images of the ultraviolet footprint of the Io flux tube (IFT) on Jupiter's upper atmosphere made with the Space Telescope Imaging Spectrograph on board the Hubble Space Telescope have been analyzed to characterize their location, morphology, and brightness distribution. The observations cover a wide range of central meridian Jovian longitudes and Io orbital positions and include north and south footprint emissions. Comparing the location of the IFT with that expected from the VIP4 model of the Jovian magnetic field, we find that the lead angle is generally not significantly different from zero in the System III longitude sector 125°–195°. Instead, the lead angles reach about 8° in the 50° sector, coinciding with a region of possible magnetic anomaly. We observe that the brightness of the main footprint shows intrinsic intensity changes that appear to be controlled by the system III longitude of Io and its position above or below the center of the torus. The size of the primary spot magnetically maps into a region varying from 1 to over 10 Io diameters in Io's orbital plane. Multiple footprints are observed with varying brightness relative to the mean spot. The number of spots is found to increase as Io gets closer to the torus outer edge facing the spots. The separation between the first and second spots is typically 1°–3° of longitude and increases when Io is displaced from the torus center in the direction of the IFT signature. These features confirm that Alfvén waves play an important role and generate energization of precipitated electrons. However, the observed variation of the FUV spot structure with Io's position appears inconsistent with models where reflections of Alfvén wings occur between the torus boundary and Jupiter's ionosphere. Instead, the multiple spots apparently correspond to electron precipitation generated by Alfvén waves reflected inside the plasma torus.
机译:总共有74的紫外图像足迹Io的磁流管(IFT)在木星的上气氛由太空望远镜成像摄谱仪哈勃太空望远镜分析了”来形容他们呢位置、形态和亮度分布。中央子午线的威风凛凛的经度和Io轨道位置和包括北部和南部碳足迹排放。界面张力与预期从VIP4模型木星磁场,我们发现角一般不明显不同系统中从零经度三世部门125°-195°。8°50°部门之际,恰逢一个地区可能的磁异常。亮度的主要足迹显示内在强度变化,似乎所控制Io系统III经度及其位置高于或低于环的中心。的主要点磁映射成一个地区不同直径从1到10的IoIo的轨道平面。观察不同亮度相对意味着现货。增加Io接近环外面临的边缘点。第一和第二点通常是1°3°从经度和增加当Io流离失所环中心的方向IFT签名。发挥重要作用并生成电子激发的沉淀。观察到的变化FUV点结构与Io的立场似乎不符合模型反映的阿尔芬翅膀发生环面边界和木星之间电离层。显然对应电子降水由阿尔芬波里反映出来等离子体环面。

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