论文标题

CA-K板和网络区域的时间和纬度变化:对子午流的影响

Temporal and latitudinal variations of Ca-K plage and network area: An implication to meridional flows

论文作者

Priyal, Muthu, Singh, Jagdev, Ravindra, Belur, Sindhuja, G.

论文摘要

在Kodeikanal天文台(KO)获得的CA-K镜头图用于使用相等的对比技术(ECT)来生成均匀的时间序列,以研究太阳层的长期和短期变化。 The percentage of plage, Enhanced network (EN), Active network (AN), and Quiet network (QN) area at various latitudes is compared with the activity at 35$^{\circ}$ latitude and also with the sunspot number for the period of 1907 -- 1984. The values of phase differences indicate that the activity begins at $\sim$45$^{\circ}$ latitude and shift progressively to the lower latitude at a speed $ \ sim $ 〜9.4〜m〜sec $^{ - 1} $的$。偏移速度逐渐减慢,并达到$ \ sim $ 〜3〜m〜sec $^{ - 1} $ at $ \ sim $ 5 $ 5 $^{\ circ} $ latitude。在55 $^{\ circ} $,65 $^{\ circ} $和75 $^{\ circ} $ latitude belts的变化之间,Ca-k活动的变化之间没有相差。分析表明,极纬度带的活性与黑子数抗相关。这项研究表明,太阳对流区可能存在多细胞子午流动模式。一种类型的细胞可以通过子午流将磁元素从中纬度传输到低纬度带,而另一种可以在极区域运行。

The Ca-K spectroheliograms obtained at the Kodaikanal observatory (KO) are used to generate a uniform time series using the equal contrast technique (ECT) to study the long and short-term variation in the solar chromosphere. The percentage of plage, Enhanced network (EN), Active network (AN), and Quiet network (QN) area at various latitudes is compared with the activity at 35$^{\circ}$ latitude and also with the sunspot number for the period of 1907 -- 1984. The values of phase differences indicate that the activity begins at $\sim$45$^{\circ}$ latitude and shift progressively to the lower latitude at a speed of $\sim$~9.4~m~sec$^{-1}$ . The shift speed slows down gradually and reaches $\sim$~3~m~sec$^{-1}$ at $\sim$5$^{\circ}$ latitude. No phase difference between the variations of Ca-K activity at 55$^{\circ}$, 65$^{\circ}$, and 75$^{\circ}$ latitude belts implies that changes in the activity are happening simultaneously. The analysis shows that the activity at polar latitude belts is anti-correlated with the sunspot number. This study indicates that a multi-cell meridional flow pattern could exist in the solar convection zone. One type of cell could transport the magnetic elements from mid-latitude to low-latitude belts through meridional flows, and the other one could be operating in the polar region.

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