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Searching for the Signature of the Magnetic Fields at the Base of the Solar Convection Zone with Solar Cycle Variations of p-Mode Travel Time

机译:利用p模式传播时间的太阳周期变化来搜索太阳对流区底部的磁场特征

摘要

[[abstract]]We study the solar cycle variations of the solar p-mode travel time for different wave packets to probe the magnetic fields at the base of the solar convection zone. We select the wave packets that return to the same spatial point after traveling around the Sun with integral number of bounces. The change in one-bounce travel time at solar maximum relative to minimum is approximately the same for all wave packets studied except a wave packet whose lower turning point is located at the base of the convection zone. This particular wave packet has an additional decrease in travel time at solar maximum relative to other wave packets. The magnitude of the additional decrease in travel time for this particular wave packet increases with solar activity. This additional decrease in travel time might be caused by the magnetic field perturbation and sound speed perturbation at the base of the convection zone. With the simplified assumption that this additional decrease is caused only by the magnetic field perturbation at the base of the convection zone, the field strength is estimated to be about (4-7) × 105 G at solar maximum if the filling factor is unity. However, the measured travel times of other wave packets propagating close to the base of the convection zone do not support this simplified interpretation.
机译:[[摘要]]我们研究了不同波包的太阳p模式传播时间的太阳周期变化,以探测太阳对流区底部的磁场。我们选择以整数个反弹数围绕太阳旅行后返回相同空间点的波包。对于所研究的所有波包,太阳最大值时一跳的传播时间相对于最小值的变化大致相同,除了波包的下拐点位于对流区的底部。相对于其他波包,该特定波包在太阳最大时的行进时间有额外的减少。该特定波包的行进时间额外减少的幅度随太阳活动而增加。传播时间的这种额外减少可能是由对流区底部的磁场扰动和声速扰动引起的。在简化的假设下,这种额外的减少仅是由对流区底部的磁场扰动引起的,如果填充因子为1,则在太阳最大时场强估计约为(4-7)×105G。但是,在对流区底部附近传播的其他波包的测量传播时间不支持这种简化的解释。

著录项

  • 作者

    Dean-Yi Chou;

  • 作者单位
  • 年度 2011
  • 总页数
  • 原文格式 PDF
  • 正文语种 [[iso]]en
  • 中图分类

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