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COMPARISON OF SOLAR SUBSURFACE FLOWS ASSESSED BY RING AND TIME-DISTANCE ANALYSES

机译:环流法和时程分析法估算太阳地下流的比较

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The solar near-surface shear layer exhibits a rich medley of flows that are now being measured by a variety of local helioseismic techniques. We present comparisons of the horizontal flows obtained with two of these techniques, ring and time-distance analyses, applied to Michelson Doppler Imager (MDI) Dynamics Program data from the years 1998 and 1999. The ring analyses use the frequencies of both/and p modes in inversions to obtain flows within the near-surface shear layer as a function of depth. The f-mode time-distance analyses make velocity inferences just beneath the photosphere. After degrading the spatial resolution of the time-distance analyses to match the coarser resolution of the ring analyses, we find that the flows deduced with the two methods are remarkably similar, with common inflow and outflow sites as well as agreement in flow direction. The flows from ring and time-distance analyses are highly correlated with each other (correlation coefficients ~0.8); direct correspondence of features in the flows is largely realized in both the quiet-Sun and magnetic active regions.
机译:太阳近地表剪切层展现出丰富的混合流动,目前正在通过各种局部高震技术进行测量。我们将比较使用环和时距分析这两种技术获得的水平流,并将其应用于1998年和1999年的迈克尔逊多普勒成像仪(MDI)动力学程序数据。环分析使用/和p的频率反演模式以获取近地表剪切层内的流量随深度的变化。 f模式时间距离分析仅在光球下面进行速度推断。在将时距分析的空间分辨率降级以匹配环分析的较粗分辨率之后,我们发现,两种方法推导的流量非常相似,具有相同的流入和流出位置,并且在流向上一致。环流和时距分析的流量高度相关(相关系数〜0.8);流的特征之间的直接对应关系在安静的太阳和磁性活动区域都得到了很大的实现。

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