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Multi-scale temporal features of the 14 July 2000 meter- wavelength dynamic radio spectrum compared with TRACE data

机译:2000年7月14日的米波长动态无线电频谱与TRACE数据的多尺度时间特征

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The 14 July 2000 (`Bastille Day') eruptive and geoeffective flare event was observed by the digital IZMIRAN radio spectrograph in the frequency range of 25–270 MHz. This instrument allowed the analysis of various features of the dynamic radio spectrum and their comparison with other observational data, in particular with development of a spectacular EUV post-eruption arcade recorded aboard the Transition Region and Coronal Explorer (TRACE). (1) A compressed multi-hour radio spectrum shows that the event caused a conspicuous weakening of the pre-existing noise storm. This phenomenon was perhaps caused by interaction of a large halo coronal mass ejection (CME), recorded by the the Large Angle and Spectroscopic Coronagraph (LASCO) aboard the Solar and Heliospheric Observatory (SOHO), with emitting coronal structures. (2) Several type II bands are present at the initial and maximum phases of the flare event. The frequency drifts of the clearest bands correspond to the estimated shock wave speed of 1100–2300 km s−1 that is comparable with the CME speed observed in the sky plane. (3) Significant broadband enhancements of the metric radio emission took place around of 10:24–10:27 UT coinciding with sharp development of the EUV arcade in the northeast direction. It appears to correspond to the intensification of the electron acceleration in a process of post-eruption loop formation. (4) The high-resolution radio spectrum revealed a superposition of numerous type III-like bursts and/or pulsations with a time scale ranging from a few seconds to several tens of seconds. These features can be attributed particularly to successive formation of new loops of the arcade and corresponding temporal fragmentation of the electron acceleration in the course of the post-eruption reconnection. In summary, the analysis demonstrates the correspondence between the multi-scale temporal features of the metric radio emission and such phenomena as the CME and post-eruption EUV arcade. Some spectra, images, and movies illustrating the event are presented also on the accompanying CD-ROM.
机译:数字IZMIRAN无线电光谱仪在25-270 MHz的频率范围内观测到2000年7月14日(“巴士底日”)爆发并发生了地球有效的耀斑事件。该仪器可以分析动态无线电频谱的各种特征,并将其与其他观测数据进行比较,特别是在过渡区和日冕探测器(TRACE)上记录下壮观的EUV喷发后拱廊的开发中。 (1)压缩的多个小时无线电频谱表明,该事件导致了先前存在的噪声风暴的明显减弱。这种现象可能是由太阳和日球天文台(SOHO)上的大角度和光谱日冕仪(LASCO)记录的大晕冠状物质抛射(CME)与发射的日冕结构相互作用所引起的。 (2)耀斑事件的初始阶段和最大阶段存在多个II型波段。最清晰频带的频率漂移对应于估计的1100–2300 km s-1 的冲击波速度,与在空中观测到的CME速度相当。 (3)公制无线电发射在宽带上的显着增强发生在UT的10:24–10:27左右,这与EUV拱廊在东北方向的急剧发展相吻合。它似乎与喷发后回路形成过程中电子加速度的增强相对应。 (4)高分辨率无线电频谱揭示了许多类III型脉冲和/或脉动的叠加,时间范围从几秒到几十秒不等。这些特征尤其可以归因于在喷发后重新连接的过程中,新的拱形回路的连续形成以及电子加速度的相应的时间碎片。总而言之,分析表明了公制无线电发射的多尺度时间特征与诸如CME和喷发后的EUV拱廊之类的现象之间的对应关系。附带的CD-ROM上也提供了一些说明事件的光谱,图像和电影。

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