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arXiv 2311.16331astro-ph.SR
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准两年振荡源区的日震学研究

Helioseismic Investigation of Quasi-biennial Oscillation Source Regions

Kiran Jain, Partha Chowdhury, Sushanta C. Tripathy

AI总结:

本文利用超过25年的日震声模频率数据,研究太阳准两年振荡的时间演化与深度分布,发现第23和24活动周QBO周期分别约为2年和3年,并指出其源区可能位于近表面以下数千公里处。

摘要:

我们利用全球振荡网络群(Global Oscillation Network Group)的声模振荡频率,研究了准两年振荡(QBOs)的时间演化。所用数据跨越超过25年,覆盖第23和第24太阳活动周以及第25活动周的上升阶段。分析表明,类QBO信号在两个活动周中均存在,但周期不同。第23活动周中的主导QBO周期约为2年,而第24活动周中约为3年。此外,准两年振荡信号仅在第23活动周的上升期和高活动期出现,并在2005年前后的下降期迅速减弱。相比之下,QBO信号贯穿整个第24活动周,从2009年持续到2017年。我们还探究了QBO信号的深度依赖性,发现在所有深度上均高度一致,仅近表面剪切层除外。对近表面剪切层的详细分析表明,QBO的源区可能位于表面以下仅数千公里的范围内。

英文摘要:

We studied the temporal evolution of quasi-biennial oscillations (QBOs) using acoustic mode oscillation frequencies from the Global Oscillation Network Group. The data used here span over more than 25 yr, covering solar cycles 23 and 24 and the ascending phase of cycle 25. The analysis reveals that the QBO-like signals are present in both the cycles, but with different periods. The dominant QBO period in cycle 23 is found to be about 2 yr while it is about 3 yr in cycle 24. Furthermore, the quasi-biennial oscillatory signals are present only during the ascending and high-activity phases of cycle 23 and quickly weaken around 2005 during the declining phase. In comparison, the QBO signals are present throughout the cycle 24, starting from 2009 to 2017. We also explored the depth dependence in QBO signals and obtained a close agreement at all depths, except in the near-surface shear layer. A detailed analysis of the near-surface shear layer suggests that the source region of QBOs is probably within a few thousand kilometers just below the surface.

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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