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木卫一的钠云

Io's Sodium Cloud.

出版信息

Science. 1984 Nov 2;226(4674):512-6. doi: 10.1126/science.226.4674.512.

Abstract

The first two-dimensional images of the source region of Io's neutral sodium cloud have been acquired by ground-based observation. Observed asymmetries in its spatial brightness distribution provide new evidence that the cloud is supplied by sodium that is ejected nonisotropically from Io or its atmosphere. Complementary, high-time-resolution, calibrated image sequences that give the first comprehensive picture of the variations of the fainter regions of the cloud extending more than 10(5) kilometers from Io were also obtained. These data demonstrate that the cloud exhibits a persistent systematic behavior coupled with Io's orbital position, a distinct "east-west orbital asymmetry," a variety of spatial morphologies, and true temporal changes. The geometric stability of the sodium source is also indicated. Isolation of the cloud's temporal changes constitutes an important milestone toward its utilization as a long-term probe of Io and the inner Jovian magnetosphere.

摘要

已通过地面观测获得了木卫一中性钠云源区的前两个二维图像。其空间亮度分布的观测不对称性提供了新的证据,表明该云由从木卫一或其大气中非各向同性喷出的钠供应。此外,还获得了互补的、高时间分辨率、校准的图像序列,这些序列首次全面展示了从木卫一延伸超过 10(5)公里的云的较暗区域的变化。这些数据表明,该云表现出与木卫一轨道位置相关的持续系统行为,明显的“东西向轨道不对称性”,多种空间形态以及真实的时间变化。钠源的几何稳定性也得到了表明。将云的时间变化分离出来,是将其用作木卫一和木星内磁层的长期探测器的重要里程碑。

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