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Observations of the sun at vacuum-ultraviolet wavelengths from space. Part I: Concepts and instrumentation

机译:在太空中从真空紫外波长观察太阳。第一部分:概念和手段

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Studies of the high-temperature solar atmosphere are to a large extent based on spectroscopic observations of emission lines and continuum radiation in the vacuum-ultraviolet (VUV) wavelength range of the electromagnetic spectrum. In addition, important contributions stem from soft X-ray measurements. Most of the VUV radiation is produced by transitions of atoms and ions. The resulting atomic and ionic spectral lines have formation temperatures between 10 000 K and 20 MK, representative of the chromosphere, transition region, corona, and solar flares. Some molecular lines and the continua originate in cooler regions of the Sun, around and below the temperature minimum between the photosphere and the chromosphere. Radiation at VUV wavelengths is strongly absorbed by the Earth's atmosphere. Consequently, it can only be detected with instruments on sounding rockets and spacecraft operating above the atmosphere. The progress in this field of research, in particular over the last 25 years, will be presented in the first part of this review by describing the concepts and instrumentation of modern spectrographs and imaging telescopes. This presentation is accompanied by some examples of high-resolution solar images and a discussion of radiometric-calibration aspects and wavelength measurements. A second part will follow in the near future, summarizing important results obtained on the plasma conditions in the solar atmosphere.
机译:高温太阳大气的研究很大程度上是基于在电磁光谱的真空-紫外线(VUV)波长范围内对发射线和连续辐射的光谱观察。此外,重要的贡献还来自软X射线测量。大部分VUV辐射是由原子和离子的跃迁产生的。所得的原子和离子光谱线的形成温度在10000 K至20 MK之间,代表色球层,过渡区,电晕和太阳耀斑。一些分子线和连续体起源于太阳的凉爽区域,在光球和色球之间的最低温度附近或低于该温度。 VUV波长的辐射被地球大气层强烈吸收。因此,只能通过在大气层上方操作的探空火箭和航天器上的仪器才能检测到它。在本研究的第一部分将通过描述现代光谱仪和成像望远镜的概念和仪器,来介绍该研究领域的进展,尤其是过去25年中的进展。该演示文稿附带了一些高分辨率太阳图像示例,并讨论了辐射校准方面和波长测量。第二部分将在不久的将来进行,总结了在太阳大气中的等离子体条件下获得的重要结果。

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