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THE GIANT FLARE OF 2004 DECEMBER 27 FROM SGR 1806-20

机译:SGR 1806-20,2004年12月27日的巨型耀斑

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The giant flare of 2004 December 27 from SGR 1806-20 represents one of the most extraordinary events captured in over three decades of monitoring the γ-ray sky. One measure of the intensity of the main peak is its effect on X- and γ-ray instruments. RHESSI, an instrument designed to study the brightest solar flares, was completely saturated for ~0.5 s following the start of the main peak. A fortuitous alignment of SGR 1806-20 near the Sun at the time of the giant flare, however, allowed RHESSI a unique view of the giant flare event, including the precursor, the main-peak decay, and the pulsed tail. Since RHESSI was saturated during the main peak, we augment these observations with Wind and RHESSI particle detector data in order to reconstruct the main peak as well. Here we present detailed spectral analysis and evolution of the giant flare. We report the identification of a relatively soft fast peak just milliseconds before the main peak, whose timescale and size scale indicate a magnetospheric origin. We present the novel detection of emission extending up to 17 MeV immediately following the main peak, perhaps revealing a highly extended corona driven by the hyper-Eddington luminosities. The spectral evolution and pulse evolution during the tail are presented, demonstrating significant magnetospheric twist during this phase, but no apparent magnetospheric evolution. Blackbody radii are derived for every stage of the flare, which show remarkable agreement despite the range of luminosities and temperatures covered. Finally, we confirm the existence of a hard afterglow emission extending up to 2.5 MeV in the hundreds of seconds following the giant flare.
机译:2004年12月27日发生在SGR 1806-20上的巨大耀斑代表了过去三十年监测γ射线天空中最不寻常的事件之一。衡量主峰强度的一种方法是它对X射线和γ射线仪器的影响。 RHESSI是一种旨在研究最亮的太阳耀斑的仪器,在主峰开始后约0.5 s内完全饱和。然而,在发生巨大耀斑时,SGR 1806-20在太阳附近的偶然对准使RHESSI可以看到巨大耀斑事件的独特视图,包括前兆,主峰衰减和脉冲尾巴。由于RHESSI在主峰期间已饱和,因此我们用Wind和RHESSI粒子检测器数据来增加这些观测值,以便重建主峰。在这里,我们介绍详细的光谱分析和巨型耀斑的演变。我们报告了在主峰之前数毫秒内识别出的一个相对较软的快速峰,其时间尺度和大小尺度表明了磁层的起源。我们提出了新的发射检测,该检测在紧随主峰后立即扩展到了17 MeV,这也许揭示了由超爱丁顿光度驱动的高度扩展的电晕。呈现了尾巴中的频谱演化和脉冲演化,表明在此阶段磁层明显扭曲,但没有明显的磁层演化。黑体半径是在火炬的每个阶段得出的,尽管亮度和覆盖的温度范围很广,但仍显示出惊人的一致性。最后,我们确认在巨大的耀斑爆发后的数百秒内,存在硬余辉发射,延伸至2.5 MeV。

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