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Studies of Magnetic Fields in the Solar Photosphere Using the Line-Ratio Method

机译:使用线比法研究太阳光层中的磁场

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The longitudinal magnetic field measured using the Fe I λ 525 and Fe Iλ 524.7 nm lines and global magnetic field of the sun differ depending on the observatory.To study the cause of these discrepancies, we calculate the H_‖(525)/H_‖(524.7) ratios for various combinations of magnetic ele-ments and compare them with the corresponding observed values. We use the standard quiet model of the solar photosphere suggesting that there are magnetic fields of different polarities in the range between zero and several kilogauss.The magnetic element distribution is found as a function of mag-netic field strength and the parameters of this distribution are determined for which the calculated H_‖(525)/H_‖(524.7) ratio agrees with the observed one.The sigma-components are found to be shifted differently for various points of the Fe I λ 525 nm profile calculated for the inhomogeneous magnetic field.The farther the point is from the line center,the larger the sigma-components shift.Such a pecu-liarity of the profiles may be responsible for the discrepancies in the measured values of the global mag-netic field obtained at different observatories. The increase in modulus of the global magnetic field during the maxima of solar activity can be due to a larger fraction of magnetic elements with kilogauss magnetic fields.
机译:使用Fe Iλ525和FeIλ524.7 nm线测量的纵向磁场和太阳的整体磁场因天文台而异。为研究这些差异的原因,我们计算了H_‖(525)/H_‖( 524.7)各种磁性元素组合的比率,并将它们与相应的观测值进行比较。我们使用太阳光球的标准安静模型,表明在零到几千高斯范围内存在不同极性的磁场,发现磁性元素的分布是磁场强度的函数,该分布的参数为确定所计算的H _''(525)/ H _''(524.7)比率与所观察到的比率相符。对于非均匀磁场计算得出的Fe Iλ525 nm轮廓的各个点,sigma分量的位移不同该点距线中心越远,西格玛分量的偏移就越大。轮廓的特殊性可能是造成在不同观测站获得的全球磁场测量值差异的原因。在太阳活动达到最大值时,总磁场模量的增加可能是由于具有千分之一高斯磁场的大部分磁性元素所致。

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