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arXiv 2610.16004astro-ph.SR
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在日球层模拟中融合CME通量绳模型与磁场 draping 效应

Integration of a CME Flux Rope Model with Magnetic Field Draping in Heliospheric Simulations

Department of Physics, University of Helsinki(赫尔辛基大学物理系)

Ranadeep Sarkar, Jens Pomoell, Emilia Kilpua, Eleanna Asvestari

AI总结:

该研究在EUHFORIA中实现新型FROST通量绳模型,融合磁场 draping 效应,通过模拟2013年4月11日CME事件验证其可显著提升ICME磁场预测精度,助力空间天气预报。

摘要:

准确预测行星际日冕物质抛射(ICME)的磁场结构仍是空间天气预报中的关键挑战。尽管已有多项使用全球MHD建模的研究,但仍难以推导能准确可靠重现CME磁场结构的通量绳解。我们提出FROST(嵌入太阳磁场的通量绳,Flux Rope embedded in the Solar Magnetic Field),这是欧洲日球层预报信息资产(EUHFORIA)框架内的新型通量绳模型实现,其特征为嵌入低日冕磁场的初始无力环形通量绳。FROST采用一种新颖的嵌入技术,可自洽地在通量绳周围生成 draping 磁场,确保CME边界处法向磁场分量的连续性。通量绳在低日冕和中日冕中的动力学由受观测到的事件运动学约束的非均匀平流求解,由此产生全局的、非环形的拉伸环状磁场结构。在日球层距离处,其演化通过EUHFORIA以MHD过程建模。我们通过模拟2013年4月11日的CME事件并将结果与1天文单位(au)处的原位磁场测量值比较,验证FROST模型实现的有效性。通量绳的模拟磁场剖面与观测值吻合度极高,磁场分量Bx的相关系数为0.64-0.93,By为0.92-0.95,Bz为0.82-0.87。这些结果表明,所提出的通量绳模型具备显著提升ICME磁场预测能力的潜力,凸显其在推进空间天气预报能力方面的巨大价值。

英文摘要:

Accurate prediction of the magnetic structure of interplanetary coronal mass ejections (ICMEs) remains a key challenge in space weather forecasting. Despite several efforts using global MHD modeling, it remains difficult to deduce a flux-rope solution that can accurately and reliably reproduce the magnetic structure of a CME. We present FROST (Flux Rope embedded in the Solar Magnetic Field), a new flux-rope model implementation within the European Heliospheric Forecast Information Asset (EUHFORIA), featuring an initially force-free toroidal flux rope embedded in the low-coronal magnetic field. FROST employs a novel embedding technique that self-consistently generates a draping magnetic field around the flux-rope, ensuring continuity of the normal magnetic field component at the CME boundary. The dynamics of the flux-rope in the low and middle corona is solved by a non-uniform advection constrained by the observed kinematics of the event. This results in a global, non-toroidal, stretched loop-like magnetic structure. At heliospheric distances, the evolution is modeled as an MHD process using EUHFORIA. We validate the FROST model implementation by simulating the CME event of 2013 April 11 and comparing the results with in situ magnetic field measurements at 1 au. The modeled magnetic field profiles of the flux-rope exhibit strong agreement with the observations, with correlation coefficients ranging from 0.64-0.93 for Bx, 0.92-0.95 for By, and 0.82-0.87 for Bz component of the magnetic field. These results demonstrate the capability of the proposed flux-rope model to significantly improve ICME magnetic field prediction, highlighting its strong potential for advancing space-weather forecasting capabilities.

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