Global Solar Photospheric and Coronal Magnetic Field over Activity Cycles 21-25

G. Petrie
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Abstract

The evolution of the global solar magnetic field from the beginning of cycle 21 (mid-1970s) until the currently-ascending cycle 25 is described using photospheric full-disk and synoptic magnetograms from NSO Kitt Peak Vacuum Telescope (KPVT) 512-channel and Spectromagnetograph (SPMG) and the Synoptic Optical Long-term Investigation of the Sun (SOLIS) Vector Spectro-Magnetograph (VSM) and Global Oscillations Network Group (GONG), and Stanford University's Wilcox Solar Observatory (WSO). The evolving strength and symmetry of the global coronal field is described by potential-field source-surface models decomposed into axisymmetric and non-axisymmetric, and even- and odd-ordered magnetic multipoles. The overall weakness of the global solar magnetic field since cycle 23 splits the 50-year observing window into the stronger, simpler, more hemispherically symmetric cycles 21 and 22 and the weaker, more complex cycles 23 and 24. An anomalously large decrease in the global solar field strength occurred during cycle 23, and an anomalously weak axial/polar field resulted from that cycle, accompanied by an anomalously weak radial interplanetary magnetic field (IMF) during cycle 23 activity minimum and a weakened radial IMF overall since cycle 23. The general long-term decline in solar field strength and the development during cycle 24 of strong swings of hemispheric and polar asymmetry are analyzed in detail, including their transfer through global coronal structural changes to dominate mean in situ interplanetary field measurements for several years. Although more symmetric than cycle 24, the rise phase of cycle 25 began with the southern leading the northern hemisphere, but the north has recovered to lead this cycle's polar field reversal. The mean polar flux (poleward of $\pm 60^{\circ}$) has reversed at each pole, so far more symmetrically than the cycle 23 and 24 polar reversals.
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第 21-25 活动周期的全球太阳光层和日冕磁场
利用来自美国国家天文台基特峰真空望远镜(KPVT)512 信道和光谱磁力仪(SPMG)以及太阳同步光学长期调查(SOLIS)矢量光谱磁力仪(VSM)和全球振荡网络组(GONG)的光层全磁盘和同步磁力图,描述了从周期 21 开始(20 世纪 70 年代中期)到目前正在上升的周期 25 期间全球太阳磁场的演变、以及斯坦福大学威尔科克斯太阳天文台(WSO)。全球日冕磁场的强度和对称性是通过势场源表面模型来描述的,该模型被分解为轴对称和非轴对称以及偶序和奇序磁多极。自周期 23 以来,全球太阳磁场的整体衰弱将 50 年的观测窗口分为较强、较简单、更半球对称的周期 21 和 22,以及较弱、较复杂的周期 23 和 24。在周期 23 期间,全球太阳磁场强度异常大幅下降,轴向/极地磁场异常减弱,同时在周期 23 活动最小值期间,径向行星际磁场异常减弱,自周期 23 以来,径向行星际磁场总体减弱。详细分析了太阳磁场强度的长期普遍下降以及周期 24 期间半球和极地不对称的强烈波动,包括它们通过全球日冕结构变化的转移,从而主导了数年的平均原地行星际磁场测量。虽然比周期 24 更对称,周期 25 的上升阶段开始时南半球领先于北半球,但北半球已恢复到引领本周期的极场逆转。平均极地通量($\pm 60^{\circ}$的极向)在两极都发生了逆转,到目前为止比周期23和24的极地逆转更加对称。
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