Modeling the Solar Wind Speed Based on Various Parameters of the Coronal Magnetic Field

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
I. A. Berezin, A. G. Tlatov
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引用次数: 0

Abstract

The Wang–Shelley–Arge (WSA) solar wind (SW) model is based on the idea that weakly expanding coronal magnetic field tubes are associated with fast SW sources and vice versa. The Flux-Tube Expansion factor (FTE) is used to determine the degree of expansion of magnetic tubes. The FTE is calculated based on a model of the coronal magnetic field, usually in the potential approximation. The second input parameter of the WSA model is the distance from the base of the magnetic tube on the photosphere to the boundary of the corresponding coronal hole (Distance to the Coronal Hole Boundary, DCHB). These two parameters of the coronal magnetic field are related empirically to the speed of the solar wind near the Sun. The WSA model has shortcomings and does not fully explain the mechanisms of SW formation. This paper presents an analysis of the degree of correlation of various parameters of the magnetic field (length of field lines, latitude of the base of field lines, etc.) with the observed velocity SW. The parameters are calculated in potential (PFSS) and nonpotential approximations based on three synoptic series of magnetographic observations: the Kislovodsk Solar Telescope for Operative Predictions (STOP), SDO/HMI, and WSO. We found that the FTE correlates relatively weakly with solar wind speed, in contrast to field line lengths and DCHB. We propose an alternative relation to the WSA model that relates the length of field lines, the DCHB, and the amplitude of the magnetic field at the source surface with the velocity SW. The presented relationship is not based on the FTE and shows a better correlation with observations compared to the WSA model. We also optimized the formula in the WSA model for the STOP magnetograph.

Abstract Image

基于日冕磁场各种参数的太阳风速度建模
Wang-Shelley-Arge (WSA)太阳风(SW)模型的基本思想是,弱膨胀的日冕磁场管与快速的 SW 源相关,反之亦然。磁通管膨胀因子(FTE)用于确定磁管的膨胀程度。FTE 是根据日冕磁场模型计算得出的,通常采用电势近似法。WSA 模型的第二个输入参数是从光球上的磁管底部到相应日冕洞边界的距离(到日冕洞边界的距离,DCHB)。根据经验,日冕磁场的这两个参数与太阳附近的太阳风速度有关。WSA 模型存在缺陷,不能完全解释 SW 的形成机制。本文分析了磁场各种参数(磁场线长度、磁场线基点纬度等)与观测到的速度 SW 的相关程度。这些参数是根据基斯洛沃茨克操作预测太阳望远镜(STOP)、SDO/HMI 和 WSO 这三个同步磁成像观测系列,以势能(PFSS)和非势能近似计算得出的。我们发现,FTE 与太阳风速度的相关性相对较弱,与场线长度和 DCHB 相反。我们提出了 WSA 模型的另一种关系,即场线长度、DCHB 和源表面磁场振幅与速度 SW 的关系。提出的关系不是基于 FTE,与 WSA 模型相比,与观测结果的相关性更好。我们还针对 STOP 磁强计优化了 WSA 模型中的公式。
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来源期刊
Geomagnetism and Aeronomy
Geomagnetism and Aeronomy Earth and Planetary Sciences-Space and Planetary Science
CiteScore
1.30
自引率
33.30%
发文量
65
审稿时长
4-8 weeks
期刊介绍: Geomagnetism and Aeronomy is a bimonthly periodical that covers the fields of interplanetary space; geoeffective solar events; the magnetosphere; the ionosphere; the upper and middle atmosphere; the action of solar variability and activity on atmospheric parameters and climate; the main magnetic field and its secular variations, excursion, and inversion; and other related topics.
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