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Fully resolved quiet-Sun magnetic flux tube observed with the Sunrise IMaX instrument

机译:用sunrise观察完全分辨的静音 - 太阳磁通管   ImaX仪器

摘要

Until today, the small size of magnetic elements in quiet Sun areas hasrequired the application of indirect methods, such as the line-ratio techniqueor multi-component inversions, to infer their physical properties. A consistentmatch to the observed Stokes profiles could only be obtained by introducing amagnetic filling factor that specifies the fraction of the observed pixelfilled with magnetic field. Here, we investigate the properties of a smallmagnetic patch in the quiet Sun observed with the IMaX magnetograph on boardthe balloon-borne telescope Sunrise with unprecedented spatial resolution andlow instrumental stray light. We apply an inversion technique based on thenumerical solution of the radiative transfer equation to retrieve thetemperature stratification and the field strength in the magnetic patch. Theobservations can be well reproduced with a one-component, fully magnetizedatmosphere with a field strength exceeding 1 kG and a significantly enhancedtemperature in the mid- to upper photosphere with respect to its surroundings,consistent with semi-empirical flux tube models for plage regions. We thereforeconclude that, within the framework of a simple atmospheric model, the IMaXmeasurements resolve the observed quiet-Sun flux tube.
机译:直到今天,安静的太阳区域中的磁性元素尺寸很小,因此需要应用间接方法(例如线比技术或多分量反演)来推断其物理性质。与观察到的斯托克斯曲线的一致性只能通过引入一个磁性填充因子来获得,该填充因子指定了观察到的像素被磁场填充的比例。在这里,我们研究了IMAX磁强仪在气球式望远镜Sunrise上观测到的,在空寂的太阳下小磁片的性质,该空前的空间分辨率和低的仪器杂散光。我们基于辐射传递方程的数值解应用反演技术来检索温度分层和磁贴片中的场强。场强超过1 kG的单组分全磁化大气层的观测结果可以很好地重现,相对于周围环境,中上层上层光层的温度明显升高,这与半经验通量管模型相对于pl石区域一致。因此,我们得出结论,在一个简单的大气模型的框架内,IMaX测量值可以解决观测到的静太阳通量管问题。

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