Physical causes and consequences of the solar magnetic activity cycle

太阳磁活动周期的物理原因和后果

• 批准号: RGPIN-2018-05278
• 负责人: Charbonneau, Paul
• 金额: $ 3.64万
• 依托单位: Université de Montréal
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2020
• 资助国家: 加拿大
• 起止时间: 2020-01-01 至 2021-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=713567
• 关键词: Physical; causes; consequences; solar; magnetic

The solar magnetic field is the energy source and dynamical driver of all physical phenomena collectively defining solar activity. The spatiotemporal evolution of the solar magnetic field, in turn, is powered by a hydromagnetic dynamo process, tapping its energy in the flow of electrically conducting fluid within the solar interior, chiefly turbulent convection and differential rotation. This flow-field interaction is a fundamentally nonlinear process, which for solar interior conditions is well-described by the magnetohydrodynamical (MHD) approximation. A very prominent evolutionary timescale is he so-called eleven year solar magnetic activity cycle, associated with the regular polarity reversals of the global solar magnetic field. This cycle modulates the frequency of all geoeffective solar eruptive phenomena, as well as radiative and particulate variability influencing the Earth's upper atmosphere and geospatial environment. Accordingly, understanding and predicting the solar magnetic activity cycle is a cornerstone of space weather research, as well as investigations of phenomena unfolding on much longer timescales (known as space climate). Over the past 15 years my research group has solidly positioned itself on the international scene, primarily through the production of the first global (3D) MHD simulations of solar convection generating regular solar-like magnetic cycles, and more recently via the successfull extensions of these simulations to observed stellar cycles in solar-type stars. Another important and recent breakthrough is the development of a hybrid dynamo model allowing to investigate self-consistently in detail the impact of evolving surface magnetism on the subsequent evolution of the magnetic cycle, an essential process towards solar data assimilation into dynamo-based cycle prediction simulations. The proposed research aims primarily at furthering our physical understanding of the solar (and stellar) magnetic activity cycle(s), primarily through global MHD simulations, but also via geometrically and dynamically simplified models allowing very long temporal integrations. Research objectives include: (1) understanding the physical mechanisms setting the magnetic cycle's period and amplitude; (2) understanding the origin of the cycle's variability, including epochs of strongly suppressed activity, such as the seventeenth century Maunder Minimum; (3) improving solar cycle forecasting schemes by data assimilation into dynamo models; (4) improving solar flare forecasting schemes by data assimilation into avalanche models for flare energy release.

太阳磁场是所有物理现象的能量来源和动力驱动器，共同定义了太阳活动。太阳磁场的时空演化反过来又是由磁流体发电机过程提供动力，利用太阳内部导电流体的流动，主要是湍流对流和差动旋转。这种流场相互作用是一个基本上非线性的过程，太阳内部的条件是很好地描述了磁流体动力学（MHD）近似。一个非常突出的演化时间尺度是所谓的11年太阳磁场活动周期，与全球太阳磁场的定期极性逆转有关。这一周期调节所有地球效应太阳喷发现象的频率，以及影响地球高层大气和地球空间环境的辐射和微粒变化。因此，了解和预测太阳磁活动周期是空间气象研究以及对在更长时间尺度上展开的现象（称为空间气候）进行调查的基石。 在过去的15年里，我的研究小组已经在国际舞台上稳固地定位了自己，主要是通过生产第一个全球（3D）MHD模拟太阳对流产生规则的类太阳磁循环，最近通过这些模拟的成功扩展到观察太阳型恒星的恒星周期。另一个重要的和最近的突破是一个混合发电机模型的发展，允许调查自相一致的详细不断变化的表面磁性的影响，随后演变的磁周期，一个必不可少的过程，太阳能数据同化到基于发电机的周期预测模拟。 拟议的研究主要旨在进一步加深我们对太阳（和恒星）磁活动周期的物理理解，主要通过全球MHD模拟，但也通过几何和动态简化模型允许非常长的时间积分。研究目标包括：（1）理解确定磁周期和振幅的物理机制;（2）理解周期变化的起源，包括强烈抑制活动的时期，如17世纪蒙德极小期;（3）通过将数据同化到发电机模型中来改进太阳周期预报方案;（4）改进耀斑预报方案，将数据同化到耀斑能量释放的雪崩模式中。