Palmerio Erika, Nieves-Chinchilla Teresa, Kilpua Emilia K J, Barnes David, Zhukov Andrei N, Jian Lan K, Witasse Olivier, Provan Gabrielle, Tao Chihiro, Lamy Laurent, Bradley Thomas J, Mays M Leila, Möstl Christian, Roussos Elias, Futaana Yoshifumi, Masters Adam, Sánchez-Cano Beatriz
Space Sciences Laboratory University of California-Berkeley Berkeley CA USA.
CPAESS University Corporation for Atmospheric Research Boulder CO USA.
J Geophys Res Space Phys. 2021 Nov;126(11):e2021JA029770. doi: 10.1029/2021JA029770. Epub 2021 Nov 3.
One of the grand challenges in heliophysics is the characterization of coronal mass ejection (CME) magnetic structure and evolution from eruption at the Sun through heliospheric propagation. At present, the main difficulties are related to the lack of direct measurements of the coronal magnetic fields and the lack of 3D in-situ measurements of the CME body in interplanetary space. Nevertheless, the evolution of a CME magnetic structure can be followed using a combination of multi-point remote-sensing observations and multi-spacecraft in-situ measurements as well as modeling. Accordingly, we present in this work the analysis of two CMEs that erupted from the Sun on April 28, 2012. We follow their eruption and early evolution using remote-sensing data, finding indications of CME-CME interaction, and then analyze their interplanetary counterpart(s) using in-situ measurements at Venus, Earth, and Saturn. We observe a seemingly single flux rope at all locations, but find possible signatures of interaction at Earth, where high-cadence plasma data are available. Reconstructions of the in-situ flux ropes provide almost identical results at Venus and Earth but show greater discrepancies at Saturn, suggesting that the CME was highly distorted and/or that further interaction with nearby solar wind structures took place before 10 AU. This work highlights the difficulties in connecting structures from the Sun to the outer heliosphere and demonstrates the importance of multi-spacecraft studies to achieve a deeper understanding of the magnetic configuration of CMEs.
日球物理学中的一大挑战是对日冕物质抛射(CME)的磁结构进行表征,并追踪其从太阳爆发到日球层传播的演化过程。目前,主要困难在于缺乏对日冕磁场的直接测量,以及在行星际空间中缺乏对CME主体的三维原位测量。尽管如此,CME磁结构的演化可以通过多点遥感观测、多航天器原位测量以及建模相结合的方式来追踪。因此,我们在这项工作中对2012年4月28日从太阳爆发的两次CME进行了分析。我们利用遥感数据追踪它们的爆发和早期演化,发现了CME - CME相互作用的迹象,然后利用金星、地球和土星的原位测量数据来分析它们在行星际空间中的对应物。我们在所有位置都观测到了一个看似单一的通量绳,但在地 球上发现了可能的相互作用迹象,因为地球上有高时间分辨率的等离子体数据。对原位通量绳的重建在金星和地球得到了几乎相同的结果,但在土星上显示出更大的差异,这表明CME在10天文单位之前就已经高度扭曲和/或与附近的太阳风结构发生了进一步的相互作用。这项工作突出了将太阳上的结构与外日球层结构联系起来的困难,并证明了多航天器研究对于更深入理解CME磁结构的重要性。