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Photospheric and coronal magnetic fields in six magnetographs - II. Harmonic scaling of field intensities

机译:六个磁强计中的光球和日冕磁场-II。场强度的谐波标度

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Context. Photospheric magnetic fields have been observed since the 1970s by several ground-based and satellite instruments. While the different instruments show a fairly similar large-scale structure and temporal evolution of the photospheric magnetic field, the magnetic field intensity varies significantly between the observations. Aims. We introduce a new method for scaling the photospheric magnetic field in terms of the harmonic expansion. Contrary to earlier scaling methods, the harmonic scaling method can be straightforwardly used for data sets of different resolutions. Methods. We use synoptic maps constructed from Wilcox Solar Observatory, Mount Wilson Observatory (MWO), Kitt Peak (KP), SOLIS, SOHO/MDI and SDO/HMI measurements of the photospheric field. We calculate the harmonic expansions of the magnetic field for all these data sets (for most, up to n = 180 ) and investigate the scaling of the harmonic coefficients between all possible pairs of data sets. Results. The six data sets generally scale to one another relatively well, with the exception of even axial terms, especially the g _(2)~(0) quadrupole for a few pairs of data sets. Differences in polar field observations, pole-filling methods and possible zero-level mainly affect the scaling of even axial terms. Scaling factors typically slightly increase with harmonic order. The mutual scaling between SOLIS and HMI is very good, and one single overall coefficient of approximately 0.8 would be a reasonable choice for those data sets. Our results suggest that the KP synoptic maps are offset by a few degrees with respect to MWO and MDI. We note that the new method gives a correct scaling for the low harmonic terms that are sufficient and necessary for coronal modeling.
机译:上下文。自1970年代以来,几种地面和卫星仪器都观测到了光球磁场。尽管不同的仪器显示出光球磁场的大规模结构和时间演化相当相似,但两次观测之间的磁场强度却有很大差异。目的我们介绍了一种根据谐波膨胀来缩放光球磁场的新方法。与早期的缩放方法相反,谐波缩放方法可以直接用于不同分辨率的数据集。方法。我们使用由威尔科克斯太阳天文台,威尔逊山天文台(MWO),基特峰(KP),SOLIS,SOHO / MDI和SDO / HMI测量的光球场构造的天气图。我们为所有这些数据集(大多数情况下,最多n = 180)计算磁场的谐波扩展,并研究所有可能的数据对对之间的谐波系数的换算。结果。除偶数轴向项外,这六个数据集通常可以很好地相互缩放,尤其是几对数据集的g_(2)〜(0)四极杆。极场观测,极点填充方法和可能的零位的差异主要影响偶数轴向项的缩放。比例因子通常随谐波次数而略微增加。 SOLIS和HMI之间的相互缩放非常好,对于这些数据集,一个整体系数大约为0.8会是一个合理的选择。我们的结果表明,相对于MWO和MDI,KP天气图偏移了几度。我们注意到,该新方法为低谐波项提供了正确的缩放比例,这对于日冕模型是足够的和必要的。

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