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Direct measurement of the formation height difference of?the?630?nm Fe?I solar lines

机译:直接测量?630nm Fe?I太阳线的形成高度差

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Context. Spectral lines formed over a limited height rangein either a stellar or planetary atmosphere provide us with informationabout the physical conditions within this height range. In thiscontext, an important quantity is the so-called line formation depth.It is usually determined from numerical calculation of the atmosphericopacity in the line of interest and then converted into geometricaldepth by using atmospheric models. Aims. We develop a radically different approach, which allows usto measure directly line formation depths from spectroscopicobservations without relying on assumptions about an atmospheric model.This method requires spatially resolved observations, which up to nowhave been available only for solar or planetary studies. We apply thismethod to images of the solar granulation. Methods. The method was presented and tested numerically inprevious papers. It is based on the measurement of the perspectiveshift between images at different wavelengths, formed at differentheights, when they are observed away from disk center. Because of theFourier transform properties, this shift gives rise to a deterministiclinear phase term in the cross spectrum of the images. Results. The method is applied to observations of solar quietregions performed with the SOT spectropolarimeter on HINODE in theFe Iline pair at 630.15 and 630.25nm.We derive the difference in formation heights between the two lines andits center-to-limb variations. We show that the high sensitivity of themeasurements allows us to detect variations in the line formationheights between magnetized and non-magnetized regions of the solaratmosphere. Conclusions. Our results are the first direct measurements ofline formation depths in the solar photosphere. Cross spectral analysisprovides us with a new observable quantity, which may be measured withan accuracy well bellow the spatial resolution of the observations. Werecall that the Fe Iline pairat630.15 and630.25nm is often used to determine solarmagnetic fields by spectropolarimetric observations and inversionmethods. The difference in the line formation heights that we measureshould be taken into account in the inversion procedures. Key words: line: formation - techniques: high angular resolution - techniques: spectroscopic - Sun: photosphere
机译:上下文。在恒星或行星大气中在有限的高度范围内形成的光谱线为我们提供了有关在此高度范围内的物理条件的信息。在这种情况下,一个重要的量就是所谓的线形成深度,通常通过对感兴趣线中大气不透明度的数值计算来确定,然后通过使用大气模型将其转换为几何深度。目的我们开发了一种截然不同的方法,该方法使我们能够从光谱观测中直接测量线层深度,而无需依赖于大气模型的假设,该方法需要空间分辨的观测值,而到目前为止,这种观测值仅可用于太阳或行星研究。我们将此方法应用于太阳造粒的图像。方法。提出了该方法并在以前的论文中进行了数值测试。它是基于在远离磁盘中心观察时,在不同高度形成的不同波长的图像之间的透视偏移的测量结果。由于傅立叶变换的特性,这种偏移在图像的交叉光谱中产生了确定性的线性相位项。结果。该方法适用于在铁Iline对中的HINODE上用SOT分光仪在630.15nm和630.25nm处进行的太阳静区观测。我们推导出两条线之间的地层高度差异及其中心到边缘的变化。我们表明测量的高灵敏度使我们能够检测到太阳大气的磁化区域和非磁化区域之间的线形成高度的变化。结论。我们的结果是对太阳光球中线形成深度的首次直接测量。互谱分析为我们提供了一个新的可观测量,可以在观测值的空间分辨率以下很好地进行测量。我们记得,通过光谱极化观测和反演方法,通常使用630.15nm和630.25nm的Fe Iline对来确定太阳磁场。在反演程序中应考虑我们测量的线形高度的差异。关键词:线:形成-技术:高角度分辨率-技术:光谱学-太阳:光球

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