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First Imaging of Coronal Mass Ejections in the Heliosphere Viewed from Outside the Sun – Earth Line

机译:从太阳-地球线以外观察到的日冕中日冕物质喷射的首次成像

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We show for the first time images of solar coronal mass ejections (CMEs) viewed using the Heliospheric Imager (HI) instrument aboard the NASA STEREO spacecraft. The HI instruments are wide-angle imaging systems designed to detect CMEs in the heliosphere, in particular, for the first time, observing the propagation of such events along the Sun – Earth line, that is, those directed towards Earth. At the time of writing the STEREO spacecraft are still close to the Earth and the full advantage of the HI dual-imaging has yet to be realised. However, even these early results show that despite severe technical challenges in their design and implementation, the HI instruments can successfully detect CMEs in the heliosphere, and this is an extremely important milestone for CME research. For the principal event being analysed here we demonstrate an ability to track a CME from the corona to over 40 degrees. The time – altitude history shows a constant speed of ascent over at least the first 50 solar radii and some evidence for deceleration at distances of over 20 degrees. Comparisons of associated coronagraph data and the HI images show that the basic structure of the CME remains clearly intact as it propagates from the corona into the heliosphere. Extracting the CME signal requires a consideration of the F-coronal intensity distribution, which can be identified from the HI data. Thus we present the preliminary results on this measured F-coronal intensity and compare these to the modelled F-corona of Koutchmy and Lamy (IAU Colloq. 85, 63, 1985). This analysis demonstrates that CME material some two orders of magnitude weaker than the F-corona can be detected; a specific example at 40 solar radii revealed CME intensities as low as 1.7×10−14 of the solar brightness. These observations herald a new era in CME research as we extend our capability for tracking, in particular, Earth-directed CMEs into the heliosphere.
机译:我们首次展示了使用NASA STEREO航天器上的日球成像仪(HI)仪器观测到的太阳日冕质量抛射(CME)的图像。 HI仪器是一种广角成像系统,设计用于特别是首次检测日球中的CME,观察此类事件沿太阳-地球线(即指向地球的事件)的传播。在撰写本文时,STEREO航天器仍靠近地球,HI双重成像的全部优势尚未实现。但是,即使是这些早期结果也表明,尽管HI仪器在设计和实施方面存在严峻的技术挑战,但它们仍可以成功地检测出太阳圈中的CME,这对于CME研究而言是极为重要的里程碑。对于这里要分析的主要事件,我们展示了一种跟踪CME从电晕到40度以上的能力。时间-高度历史显示,至少在前50个太阳半径上,上升速度是恒定的,并且有一些证据表明,距离超过20度时减速。对相关的日冕仪数据和HI图像的比较表明,CME的基本结构在从日冕传播到日球层时仍保持完好无损。提取CME信号需要考虑F冠状强度分布,这可以从HI数据中识别出来。因此,我们提出了关于该测得的F冠冕强度的初步结果,并将其与Koutchmy和Lamy的模拟F冠冕进行了比较(IAU Colloq。85,63,1985)。该分析表明,可以检测到比F-电晕弱两个数量级的CME材料。一个在太阳半径为40的特定示例显示CME强度低至太阳亮度的1.7×10 −14 。这些观测结果预示着CME研究的新纪元,因为我们扩展了跟踪能力,尤其是将地球定向CME跟踪到太阳圈的能力。

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