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Multi-source Connectivity As the Driver of Solar Wind Variability in the Heliosphere

Nature Astronomy(2024)

Northumbria Univ | George Mason Univ | INAF Ist Astrofis & Planetol Spaziali | UCL | Dublin City Univ | Univ Paris Diderot | Univ Reading | Univ Michigan | European Space Agcy | Inst Rech Astrophys & Planetol | UKRI STFC Rutherford Appleton Lab | World Radiat Ctr | Max Planck Inst Sonnensyst Forsch

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Abstract
The ambient solar wind that fills the heliosphere originates from multiple sources in the solar corona and is highly structured. It is often described as high-speed, relatively homogeneous, plasma streams from coronal holes and slow-speed, highly variable, streams whose source regions are under debate. A key goal of ESA/NASA's Solar Orbiter mission is to identify solar wind sources and understand what drives the complexity seen in the heliosphere. By combining magnetic field modelling and spectroscopic techniques with high-resolution observations and measurements, we show that the solar wind variability detected in situ by Solar Orbiter in March 2022 is driven by spatio-temporal changes in the magnetic connectivity to multiple sources in the solar atmosphere. The magnetic field footpoints connected to the spacecraft moved from the boundaries of a coronal hole to one active region (12961) and then across to another region (12957). This is reflected in the in situ measurements, which show the transition from fast to highly Alfv & eacute;nic then to slow solar wind that is disrupted by the arrival of a coronal mass ejection. Our results describe solar wind variability at 0.5 au but are applicable to near-Earth observatories. Solar wind is highly structured yet variable. Close-up observations of the solar atmosphere reveal that the changing connectivity of multiple sources in the solar corona drives the observed complexity and variability in the inner heliosphere.
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要点】:该论文指出,2022年3月Solar Orbiter任务在太空中检测到的太阳风变异性,是由太阳大气层多个源头的磁连接性时空变化所驱动的,这一发现突显了太阳风复杂性的驱动因素。

方法】:研究结合了磁场建模、光谱技术、高分辨率观测和测量。

实验】:通过Solar Orbiter在2022年3月的现场测量,观察到连接到磁场的足点从冕洞边界移动到一个活动区域(12961),然后再到另一个区域(12957),从而在现场测量中显示了从快速到高度 Alfvénic 然后到由日冕物质抛射打断的缓慢太阳风的转变。