光球直射无日冕建模的开放式太阳通量

Ismo Tähtinen, Timo Asikainen, Kalevi Mursula
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引用次数: 0

摘要

开放的太阳磁通量,即从太阳逸出的总磁通量,是将太阳活动与地球联系起来的最重要参数之一。然而,开阔太阳磁通量与光球磁场分布的直接关系如何这一问题仍有部分未知。我们的目标是在不对日冕做任何假设和不使用日冕洞观测数据的情况下,直接根据光球磁场重建开阔太阳通量。我们修改了早期的矢量求和方法,将磁场极性考虑在内,并将该方法应用于六台仪器的同步磁图,以确定太阳周期 21-24 的开日磁通量。结果。修改后的矢量求和法产生了一个全球太阳磁场矢量,其大小与来自势场源表面(PFSS)模型的开放太阳磁通量在绝对尺度和六个磁图中每个磁图的整体时间演变上都非常吻合。该矢量的纬度遵循黑尔周期,始终指向正极性占主导地位的半球,其经度与麦金托什档案中主要日冕洞的位置一致。通过将该矢量的大小与PFSS模型计算出的不同源表面高度的开放太阳通量进行比较,我们发现源表面高度为$R_{ss} = 2.4 -2.5R_\odot$时匹配度最高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Straight outta photosphere: Open solar flux without coronal modeling
The open solar flux, that is, the total magnetic flux escaping the Sun, is one of the most important parameters connecting solar activity to the Earth. The open solar flux is commonly estimated from photospheric magnetic field measurements by making model assumptions about the solar corona. However, the question in which way the open solar flux is directly related to the distribution of the photospheric magnetic field is still partly unknown. We aim to reconstruct the open solar flux directly from the photospheric magnetic fields without making any assumptions about the corona and without using coronal hole observations, for instance. We modified an earlier vector sum method by taking magnetic field polarities into account and applied the method to the synoptic magnetograms of six instruments to determine the open solar flux from solar cycles 21-24. Results. The modified vector sum method produces a vector of the global solar magnetic field whose magnitude closely matches the open solar flux from the potential field source surface (PFSS) model both by the absolute scale and the overall time evolution for each of the six magnetograms. The latitude of this vector follows the Hale cycle by always pointing toward the dominantly positive-polarity hemisphere, and its longitude coincides with the location of the main coronal holes of the McIntosh Archive. We find multi-year periods during which the longitude of the vector slowly drifts or stays rather stationary in the Carrington frame. These periods are punctuated by times when the longitude moves rapidly in the Carrington frame. By comparing the magnitude of this vector to the open solar flux calculated from the PFSS model with different source surface heights, we find that the best match is produced with a source surface height $R_{ss} = 2.4 - 2.5R_\odot$.
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