论文标题

从遥感数据中得出CME密度,并与原位测量值进行比较

Deriving CME density from remote sensing data and comparison to in-situ measurements

论文作者

Temmer, M., Holzknecht, L., Dumbovic, M., Vrsnak, B., Sachdeva, N., Heinemann, S. G., Dissauer, K., Scolini, C., Asvestari, E., Veronig, A. M., Hofmeister, S. J.

论文摘要

我们使用合并的立体声 - 苏荷州白色光数据确定了29个观察到的冠状质量弹出(CME)及其行星际对应物(ICME)的3D几何形状和depRodent质量。从几何参数中,我们计算了磁性喷射(通量杆型几何形状)和鞘结构(类似壳的几何形状)的CME的体积。在假设CME质量大致分布在特定体积内的假设下,我们会自相似地扩展CME,并计算靠近太阳(15-30 rs)和1AU的距离的CME密度。 Specific trends are derived comparing calculated and in-situ measured proton densities at 1AU, though large uncertainties are revealed due to the unknown mass and geometry evolution: i) a moderate correlation for the magnetic structure having a mass that stays rather constant (~0.56-0.59), and ii) a weak correlation for the sheath density (~0.26) by assuming the sheath region is an extra mass - as expected for a mass堆积工艺 - 与初始CME depRexted质量相当。高度相关性是在原位测得的鞘密度与太阳风密度(〜 -0.73)和太阳风速(〜0.56)之间得出的,因为在干扰到达前24小时后测量。这提供了额外的确认,即鞘等鞘确实源于堆积的太阳能风料。尽管CME星际繁殖速度与鞘密度无关,但CME的大小可能在可以堆积多少材料方面起作用。

We determine the 3D geometry and deprojected mass of 29 well-observed coronal mass ejections (CMEs) and their interplanetary counterparts (ICMEs) using combined STEREO-SOHO white-light data. From the geometry parameters we calculate the volume of the CME for the magnetic ejecta (flux-rope type geometry) and sheath structure (shell-like geometry resembling the (I)CME frontal rim). Working under the assumption that the CME mass is roughly equally distributed within a specific volume, we expand the CME self-similarly and calculate the CME density for distances close to the Sun (15-30 Rs) and at 1AU. Specific trends are derived comparing calculated and in-situ measured proton densities at 1AU, though large uncertainties are revealed due to the unknown mass and geometry evolution: i) a moderate correlation for the magnetic structure having a mass that stays rather constant (~0.56-0.59), and ii) a weak correlation for the sheath density (~0.26) by assuming the sheath region is an extra mass - as expected for a mass pile-up process - that is in its amount comparable to the initial CME deprojected mass. High correlations are derived between in-situ measured sheath density and the solar wind density (~ -0.73) and solar wind speed (~0.56) as measured 24 hours ahead of the arrival of the disturbance. This gives additional confirmation that the sheath-plasma indeed stems from piled-up solar wind material. While the CME interplanetary propagation speed is not related to the sheath density, the size of the CME may play some role in how much material could be piled up.

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