The operationally ready full three-dimensional magnetohydrodynamic (3D MHD) model from the Sun to Earth: COCONUT+Icarus

Tinatin Baratashvili, Michaela Brchnelova, Luis Linan, Andrea Lani, Stefaan Poedts
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Abstract

Solar wind modelling has become a crucial area of study due to the increased dependence of modern society on technology, navigation, and power systems. Accurate space weather forecasts can predict upcoming threats to Earth's geospace. In this study, we examine a novel full magnetohydrodynamic (MHD) chain from the Sun to Earth. The goal of this study is to demonstrate the capabilities of the full MHD modelling chain from the Sun to Earth by finalising the implementation of the full MHD coronal model into the COolfluid COroNa UnsTructured (COCONUT) model and coupling it to the MHD heliospheric model Icarus. The resulting coronal model has significant advantages compared to the pre-existing polytropic alternative, as it models a more realistic bi-modal wind, which is crucial for heliospheric studies. In this study, only thermal conduction, radiative losses, and approximated coronal heating function were considered in the energy equation. A realistic specific heat ratio was applied. The output of the coronal model was used to onset the 3D MHD heliospheric model Icarus. A minimum solar activity case was chosen as the first test case for the full MHD model. The numerically simulated data in the corona and the heliosphere were compared to observational products. We present a first attempt to obtain the full MHD chain from the Sun to Earth with COCONUT and Icarus. The coronal model has been upgraded to a full MHD model for a realistic bi-modal solar wind configuration. The approximated heating functions have modelled the wind reasonably well, but simple approximations are not enough to obtain a realistic density-speed balance or realistic features in the low corona and farther, near the outer boundary. The full MHD model was computed in 1.06 h on 180 cores of the Genius cluster of the Vlaams Supercomputing Center, which is only 1.8 times longer than the polytropic simulation.
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可运行的从太阳到地球的全三维磁流体动力学(3D MHD)模型:COCONUT+Icarus
由于现代社会对技术、导航和电力系统的依赖性日益增加,太阳风建模已成为一个重要的研究领域。准确的空间天气预报可以预测地球空间即将面临的威胁。在本研究中,我们研究了从太阳到地球的新型全磁流体动力(MHD)链。本研究的目标是通过将完整的 MHD 日冕模型最终实施到 COolfluidCOroNa UnsTructured(COCONUT)模型中,并将其与 MHD 日光层模型 Icarus 相耦合,展示从太阳到地球的完整 MHD 建模链的能力。由此产生的日冕模型与先前存在的多向性替代模型相比具有显著优势,因为它模拟了更真实的比模式风,这对日光层研究至关重要。在这项研究中,能量方程只考虑了热传导、辐射损失和近似日冕加热函数。采用的是符合实际的特定热比。日冕模型的输出被用于建立三维 MHD 日光层模型 Icarus。选择太阳活动最小的情况作为完整 MHD 模型的第一个测试案例。我们首次尝试利用 COCONUT 和 Icarus 获得从太阳到地球的完整 MHD 链。我们首次尝试利用 COCONUT 和 Icarus 获得从太阳到地球的完整 MHD 链。日冕模型已经升级为一个完整的 MHD 模型,用于现实的双模太阳风配置。近似加热函数对风的模拟相当好,但简单的近似值不足以获得逼真的密度-速度平衡或低日冕和更远的外边界附近的逼真特征。完整的 MHD 模型在弗拉芒超级计算中心 Genius 集群的 180 个内核上只用了 1.06 小时就完成了计算,这比多向模拟只用了 1.8 倍的时间。
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