arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 2003.10851astro-ph.SRphysics.space-ph
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质子-质子碰撞年龄对太阳风类型的排序

Proton-proton collisional age to order solar wind types

Verena Heidrich-Meisner, Lars Berger, Robert F. Wimmer-Schweingruber

摘要:

太阳风流的性质是由它的源区和传输效应决定的。与太阳风类型无关,现场测量的太阳风总是受到两者的影响。我们考虑质子-质子碰撞年龄作为1 AU处太阳风的排序参数,并探讨其与Xu & Borovsky(2015)开发的太阳风分类方案的关系。我们用这个来表明,明确的磁场信息是不需要这种太阳风分类。基于这一分类的三种基本太阳风类型涵盖不同的质子-质子碰撞年龄$a_{col,p-p}$方面的制度的观察,我们提出了一个简化的太阳风分类方案,仅基于质子-质子碰撞年龄。由此产生的所谓PAC太阳风分类器是完整的Xu & Borovsky(2015)太阳风分类方案的替代方案,并导致与完整的Xu & Borovsky(2015)方案非常相似的分类。质子-质子碰撞年龄使太阳风有序化。这意味着潜在的内在关系的等离子体属性,特别是质子温度和磁场强度在每个等离子体制度。我们认为,扇区反转等离子体是一个组合,特别缓慢和密集的太阳风和大多数流相互作用的边界。大多数太阳风参数(例如,磁场强度B和氧电荷状态比$n_{O^{7+}}$ / $n_{O^{6+}}$)随太阳活动周期而变化。因此,所有基于阈值的太阳风分类方案也需要适应太阳活动周期。

英文摘要:

The properties of a solar wind stream are determined by its source region and by transport effects. Independently of the solar wind type, the solar wind measured in situ is always affected by both. We consider the proton-proton collisional age as an ordering parameter for the solar wind at 1AU and explore its relation to the solar wind classification scheme developed by Xu & Borovsky (2015). We use this to show that explicit magnetic field information is not required for this solar wind classification. Based on the observation that the three basic solar wind types from this categorization cover different regimes in terms of proton-proton collisional age $a_{col,p-p}$ , we propose a simplified solar wind classification scheme that is only based on the proton-proton collisional age. The resulting so-called PAC solar wind classifier is an alternative to the full Xu & Borovsky (2015) solar wind classification scheme and leads to a classification that is very similar to the full Xu & Borovsky (2015) scheme. The solar wind is well ordered by the proton-proton collisional age. This implies underlying intrinsic relationships between the plasma properties, in particular, proton temperature and magnetic field strength in each plasma regime. We argue that sector-reversal plasma is a combination of particularly slow and dense solar wind and most stream interaction boundaries. Most solar wind parameters (e.g., the magnetic field strength, B, and the oxygen charge state ratio $n_{O^{7+}}$ /$n_{O^{6+}}$) change with the solar activity cycle. Thus, all solar wind categorization schemes based on threshold values need to be adapted to the solar activity cycle as well.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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