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首页> 外文期刊>The Astrophysical journal >RING ANALYSIS OF SOLAR SUBSURFACE FLOWS AND THEIR RELATION TO SURFACE MAGNETIC ACTIVITY
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RING ANALYSIS OF SOLAR SUBSURFACE FLOWS AND THEIR RELATION TO SURFACE MAGNETIC ACTIVITY

机译:太阳表面流的环分析及其与表面磁活动的关系

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摘要

We measure the horizontal flows in the outer 2% of the Sun by analyzing 14 consecutive Carrington rotations of Global Oscillation Network Group (GONG) Doppler images and two of Michelson Doppler Imager (MDI) Dynamics Program data with the ring-diagram technique. The zonal and meridional flows show no variation with activity at low to medium activity levels (below 71 G). At active region locations, the zonal flow increases with increasing activity; active regions rotate faster than their quieter surroundings. The meridional flow at active region locations is more equatorward than on average at depths less than about 10 Mm; the flow converges toward the mean latitude of activity. At depths greater than about 10 Mm, some active region locations show poleward and others equatorward motions indicating strong outflows from active regions. The estimated vertical flow decreases with increasing activity levels except at active region locations at depths greater than about 10 Mm; active regions show downflows near the surface and upflows at depths greater than about 10 Mm. The velocity errors increase somewhat with increasing activity at flux levels below 71 G, but they increase rapidly up to about 2 times the median error at higher flux values. This increase occurs at all depths. The flows averaged over all longitudes show the patterns expected from solar cycle variations. The quiet and the intermediate activity subsets show the same flow pattern, while the active region subset shows a mixture of solar cycle flow pattern and local flow behavior.
机译:通过使用环形图技术分析全球振荡网络组(GONG)多普勒图像的连续14次Carrington旋转和两个迈克尔逊多普勒成像器(MDI)动力学程序数据,我们测量了太阳外部2%的水平流动。在中低活动水平(71 G以下)下,纬向和经向流量都没有变化。在活动区域​​位置,地带流量随活动增加而增加。活动区域的旋转速度比周围安静的区域快。在活动区域​​位置的子午流比平均深度小于约10 Mm的赤道流要平均。流量收敛到平均活动纬度。在大于约10 Mm的深度处,一些活动区域位置显示极极运动,而其他赤道运动则显示有大量活动区域流出。除了活动深度大于10 Mm的活动区域位置以外,估计的垂直流量随活动水平的增加而减小;活跃区域显示出地表附近的向下流动和深度大于约10 Mm的向上流动。在低于71 G的通量水平下,速度误差随活性的增加而有所增加,但在较高的通量值下,它们会迅速增加至中值误差的2倍左右。这种增加发生在所有深度。所有经度上的平均流量显示了太阳周期变化所预期的模式。安静和中间活动子集显示相同的流动模式,而活动区域子集显示太阳周期流动模式和局部流动行为的混合。

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