arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 1502.07607astro-ph.SR
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根据18年GOLF/SoHO观测对地表下太阳活动的地震灵敏度

Seismic sensitivity to sub-surface solar activity from 18 years of GOLF/SoHO observations

D. Salabert, R. A. Garcia, S. Turck-Chieze

摘要:

太阳活动在过去的两个施瓦贝周期中发生了显着变化。在第23个周期结束时经历了一个漫长而深刻的最小值之后,第24个周期的活动较弱,与前几个周期形成对比。在这项工作中,太阳声振荡对太阳活动的响应,以提供见解的结构和磁变化在太阳的次表层在这一持续不寻常的低活动期。我们分析了18年的连续观测太阳声振荡收集的太阳作为一个明星GOLF仪器SoHO航天器。从拟合的模式频率,径向,偶极,和四极模式的频率偏移的时间变化的研究对于不同的频率范围,这是敏感的太阳次表面内部的不同层。低频模式在第23和24周期之间显示出几乎不变的频率偏移,具有准两年振荡的时间演变特征,这对于揭示复杂磁结构存在的四极分量特别明显。在循环~24期间,较高频率下的模式显示频率偏移小30%,这与在循环23和24之间观察到的表面活性降低一致。18年的GOLF振荡的分析表明,结构和磁场的变化负责的频率变化保持可比的周期23和周期24之间在更深的次表层低于1400公里的低频模式所揭示的。高频模式的频移,对较浅的区域敏感,表明第24周在太阳上层的磁性较弱。

英文摘要:

Solar activity has significantly changed over the last two Schwabe cycles. After a long and deep minimum at the end of Cycle 23, the weaker activity of Cycle 24 contrasts with the previous cycles. In this work, the response of the solar acoustic oscillations to solar activity is used in order to provide insights on the structural and magnetic changes in the sub-surface layers of the Sun during this on-going unusual period of low activity. We analyze 18 years of continuous observations of the solar acoustic oscillations collected by the Sun-as-a-star GOLF instrument onboard the SoHO spacecraft. From the fitted mode frequencies, the temporal variability of the frequency shifts of the radial, dipolar, and quadrupolar modes are studied for different frequency ranges which are sensitive to different layers in the solar sub-surface interior. The low-frequency modes show nearly unchanged frequency shifts between Cycles 23 and 24, with a time evolving signature of the quasi-biennial oscillation, which is particularly visible for the quadrupole component revealing the presence of a complex magnetic structure. The modes at higher frequencies show frequency shifts 30% smaller during Cycle~24, which is in agreement with the decrease observed in the surface activity between Cycles 23 and 24. The analysis of 18 years of GOLF oscillations indicates that the structural and magnetic changes responsible for the frequency shifts remained comparable between Cycle 23 and Cycle 24 in the deeper sub-surface layers below 1400 km as revealed by the low-frequency modes. The frequency shifts of the higher-frequency modes, sensitive to shallower regions, show that Cycle 24 is magnetically weaker in the upper layers of Sun.

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