Voyager's observations in the vicinity of the heliopause

IF 0.5 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
R. Caballero, J. Richardson
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引用次数: 0

Abstract

This work analyzes Voyager 2 observations on November 2018 and compares them with Voyager 1 data at the vicinity of the heliopause in July-August 2012. We describe the plasma and cosmic-ray variations at the radial distance of $\approx$ 1 astronomical unit (AU) from the heliopause. We use a simple convection-diffusion cosmic-ray modulation model to qualitatively explain the particle observations. We found a thin layer, with a thickness of $\approx$ 0.04 AU where the radial component of the solar wind speed vanished, the galactic cosmic ray intensity rapidly increased to reach its heliosphere boundary level, and low-energy heliospheric ion intensity drooped. We called this layer the "skin of the heliosphere". Plasma data suggest that Voyager 2 crossed the heliopause on November 5, 2018, at the radial distance of 119.03 AU. We apply our analysis to Voyager 1 observations and conclude that similar behavior in solar wind speed could qualitatively explain the GCR counting rate and that the "skin of the heliosphere" maybe a global characteristic along the heliopause.
旅行者号在日顶附近的观测
这项工作分析了2018年11月旅行者2号的观测结果,并将其与2012年7月至8月旅行者1号在日顶附近的数据进行了比较。我们描述了在距离日顶$\approxy$1天文单位(AU)的径向距离处的等离子体和宇宙射线的变化。我们使用一个简单的对流-扩散宇宙射线调制模型来定性地解释粒子观测。我们发现了一层厚度约为$0.04 AU的薄层,其中太阳风速的径向分量消失,银河系宇宙射线强度迅速增加,达到日球层边界水平,低能日球层离子强度下降。我们称这层为“日球层的表皮”。等离子体数据表明,旅行者2号于2018年11月5日以119.03 AU的径向距离穿过日顶。我们将我们的分析应用于旅行者1号的观测,得出结论,太阳风速的类似行为可以定性地解释GCR计数率,“日球层的表皮”可能是日顶的一个全球特征。
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来源期刊
Geofisica Internacional
Geofisica Internacional 地学-地球化学与地球物理
CiteScore
1.00
自引率
0.00%
发文量
23
审稿时长
>12 weeks
期刊介绍: Geofísica internacional is a quarterly scientific journal that publishes original papers that contain topics that are interesting for the geophysical community. The journal publishes research and review articles, brief notes and reviews books about seismology, volcanology, spacial sciences, hydrology and exploration, paleomagnetism and tectonic, and physical oceanography.
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