论文标题

计数和跟踪极性外观演变的两种新方法

Two New Methods for Counting and Tracking the Evolution of Polar Faculae

论文作者

Hovis-Afflerbach, Beryl, Pesnell, W. Dean

论文摘要

极性面孔(PFE)是太阳极线附近的磁场线的脚点,这些磁场线被视为沿颗粒边缘的明亮区域。已显示PFE数量的时间变化与极性磁场的强度相关,并成为随后的太阳周期的预测指标。由于这些特征的尺寸较小和瞬态性质,再加上不同的技术和观察因素,因此以前的PFE计数在幅度上有所不同。此外,没有可扩展的技术来衡量FACULAE的统计特性。使用Helioseisic和磁成像仪(HMI)的数据,太阳能动力学天文台(SDO),我们提出了两种跟踪Faculae和测量其性质的新方法。首先,我们在一天内计算HMI图像的标准偏差,从而将面孔视为条纹。通过将角条纹长度除以纬度依赖性旋转速率,可以找到面部寿命。我们将此方法应用于11年的134天数据。面部寿命的分布平均为6.0小时,FWHM为5.4小时,并且偏向更长的寿命,其中一些持续时间长达1天。在第二种方法中,我们用HMI磁图覆盖了渐进标准偏差的图像,以显示面部候选者与磁场之间的密切关系。结果使我们能够区分由于太阳旋转而导致的运动和由于套管在太阳表面移动而引起的“正确运动”,这证实了PFE参与极点的对流运动。使用这两种方法的PFE计数与太阳周期和极性磁场的变化中的先前计数一致。这些方法可以扩展以自动化PFE其他特性的识别和测量,这将允许自2010年SDO开始运行以来的所有faculae每日测量。

Polar faculae (PFe) are the footpoints of magnetic field lines near the Sun's poles that are seen as bright regions along the edges of granules. The time variation in the number of PFe has been shown to correlate with the strength of the polar magnetic field and to be a predictor of the subsequent solar cycle. Due to the small size and transient nature of these features, combined with different techniques and observational factors, previous counts of PFe differ in magnitude. Further, there were no scalable techniques to measure the statistical properties of faculae. Using data from the Helioseismic and Magnetic Imager (HMI) onboard the Solar Dynamics Observatory (SDO), we present two new methods for tracking faculae and measuring their properties. In the first, we calculate the standard deviation of the HMI images over one day, visualizing the faculae as streaks. The facular lifetime is found by dividing the angular streak length by the latitude-dependent rotation rate. We apply this method to 134 days of data over 11 years. The distribution of facular lifetimes has a mean of 6.0 hours, a FWHM of 5.4 hours, and a skew towards longer lifetimes, with some lasting up to 1 day. In the second method, we overlay images of the progressive standard deviation with the HMI magnetogram to show the close relationship between facular candidates and the magnetic field. The results allow us to distinguish between motion due to the Sun's rotation and "proper motion" due to faculae moving across the Sun's surface, confirming that PFe participate in convective motions at the poles. Counts of PFe using both methods agree with previous counts in their variation with the solar cycle and the polar magnetic field. These methods can be extended to automate the identification and measurement of other properties of of PFe, which would allow for daily measurements of all faculae since SDO began operation in 2010.

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