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首页> 外文期刊>The Astrophysical journal >MERIDIONAL CIRCULATION VARIABILITY FROM LARGE-APERTURE RING-DIAGRAM ANALYSIS OF GLOBAL OSCILLATION NETWORK GROUP AND MICHELSON DOPPLER IMAGER DATA
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MERIDIONAL CIRCULATION VARIABILITY FROM LARGE-APERTURE RING-DIAGRAM ANALYSIS OF GLOBAL OSCILLATION NETWORK GROUP AND MICHELSON DOPPLER IMAGER DATA

机译:全球震荡网络群和米歇尔·多普勒IMAGER数据的大孔径环图分析的子午环流变化

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Ring-diagram analysis, a local helioseismology technique, has proven to be very useful for studying solar subsurface velocity flows down to a depth of about 0.97 solar radius. The depth range is determined by the modes used in this type of analysis, and thus depends on the size of the area analyzed. Extending the area allows us to detect lower spherical harmonic degree (l) modes which, at a constant frequency, penetrate deeper in the Sun. However, there is a compromise between the size of the area and the validity of the plane-wave approximation used by the technique. We present the results of applying the ring diagrams to 30° diameter areas over the solar surface in an attempt to reach deeper into the solar interior. Meridional flows for 25 consecutive Carrington rotations (1985-2009) are derived by applying this technique to Global Oscillation Network Group (GONG) and Michelson Doppler Imager (MDI) data. This covers a time span of almost 2 yr, starting at the beginning of 2002. The amplitude of the meridional flow shows a variation of the order of 5 m s~(-1) during this period. Our results indicate that the flows increase toward the interior of the Sun for the depth range studied. We find a 1 yr periodicity in the appearance of an equa-torward meridional cell at high latitudes that coincides with maximum values of the solar inclination toward the Earth (B_0 angle).
机译:环形图分析是一种当地的地震学技术,已被证明对于研究太阳下表面流速下降到约0.97太阳半径的深度非常有用。深度范围由此类分析中使用的模式确定,因此取决于所分析区域的大小。扩展该区域使我们能够检测较低的球谐度(l)模式,这些模式以恒定的频率穿透更深的太阳。但是,在区域的大小和该技术使用的平面波近似的有效性之间存在折衷。我们提出将环图应用于太阳表面上30°直径区域的结果,以尝试更深入地进入太阳内部。通过将此技术应用于全球振荡网络组(GONG)和迈克尔逊多普勒成像仪(MDI)数据,可以得出连续25次卡灵顿旋转(1985-2009年)的子午流。从2002年初开始,这几乎涵盖了2年的时间跨度。子午流的振幅在此期间显示出5 m s〜(-1)的量级变化。我们的结果表明,在所研究的深度范围内,流向太阳内部的流量增加。我们发现在高纬度的赤道子午线细胞的出现周期为1年,该周期与太阳向地球倾斜的最大值(B_0角)一致。

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