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CORONAL SEISMOLOGY USING EIT WAVES: ESTIMATION OF THE CORONAL MAGNETIC FIELD STRENGTH IN THE QUIET SUN

机译:利用EIT波进行日冕地震学:估算安静太阳下的日冕磁场强度

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Coronal EIT waves have been observed for many years. The nature of EIT waves is still contentious, however, there is strong evidence that some of them might be fast magnetosonic waves, or at least have a fast magnetosonic wave component. The fast magnetosonic wave speed is formed from two components; the Alfvén speed (magnetic) and the sound speed (thermal). By making measurements of the wave speed, coronal density and temperature it is possible to calculate the quiet-Sun coronal magnetic field strength through coronal seismology. In this paper, we investigate an EIT wave observed on 2009 February 13 by the SECCHI/EUVI instruments on board the STEREO satellites. The wave epicenter was observed at disk center in the STEREO B (Behind) satellite. At this time, the STEREO satellites were separated by approximately 90°, and as a consequence the STEREO A (Ahead) satellite observed the wave on the solar limb. These observations allowed us to make accurate speed measurements of the wave. The background coronal density was derived through Hinode/Extreme-ultraviolet Imaging Spectrometer observations of the quiet Sun and the temperature was estimated through the narrow temperature response in the EUVI bandpasses. The density, temperature, and speed measurements allowed us to estimate the quiet-Sun coronal magnetic field strength to be approximately 0.7 ± 0.7 G.
机译:多年来已经观察到冠状EIT波。 EIT波的性质仍然存在争议,但是,有充分的证据表明,其中的一些可能是快速的磁声波,或者至少具有快速的磁声波分量。快速的磁声波速度由两个部分组成: Alfvén速度(磁性)和声速(热)。通过测量波速,日冕密度和温度,可以通过日冕地震学计算出安静的太阳日冕磁场强度。在本文中,我们调查了SECEO / EUVI仪器在STEREO卫星上于2009年2月13日观测到的EIT波。在STEREO B(后面)卫星的磁盘中心观测到了震中波。此时,STEREO卫星相隔约90°,因此STEREO A(超前)卫星观测到了太阳肢上的电波。这些观察使我们能够对波进行精确的速度测量。背景日冕密度是通过Hinode /极紫外成像光谱仪观察到的安静太阳得出的,而温度是通过EUVI带通中狭窄的温度响应来估算的。密度,温度和速度测量结果使我们能够估计出安静的太阳日冕磁场强度约为0.7±0.7G。

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