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Evolution of Magnetic Nonpotentiality in NOAA AR 9077

机译:NOAA AR 9077中磁非势的演变

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摘要

Based on photospheric vector magnetograms obtained at Huairou Solar Observing Station, we have studied the evolution of magnetic nonpotentiality in NOAA AR 9077 from 11 to 15 July 2000. We focus our analysis on the daily change of nonpotential characteristics in the photospheric magnetic field preceding the `Bastille Day' flare. We have identified the following evolving patterns: (1) The shear-angle distribution underwent dramatic change in the filament channel. At a key site of the filament environment, the magnetic shear changed sign from positive to negative. (2) The old current systems disrupted, and new but weaker systems formed before this major event. Similar changes are identified for the longitudinal current helicity. (3) The source field weakened before the flare, and the density of free magnetic energy decreased at the photospheric level. These obvious changes lasted at least nine hours before the `Bastille Day' flare, and they took place where a large amount of magnetic flux disappeared in magnetic flux cancellation. The site of dramatic changes is also found to coincide with the base of helical magnetic ropes which were seen in a 3-D force-free reconstruction. We suggest that the observed evolution of the magnetic nonpotentiality represents a continuous transportation of magnetic energy and complexity from the lower atmosphere to the corona. This transportation seems to be responsible for the energy build-up for the major flare. Moreover, the slow magnetic reconnection in the lower atmosphere, observed as magnetic flux cancellation, appears to play a key role in this energy build-up process.
机译:根据在怀柔太阳观测站获得的光球矢量磁图,我们研究了2000年7月11日至15日NOAA AR 9077中磁非势的演变。我们着重分析了在`之前的光球磁场中非势特征的日变化。巴士底日的耀斑。我们确定了以下演变模式:(1)剪切角分布在长丝通道中发生了显着变化。在灯丝环境的关键部位,磁剪切将符号从正变为负。 (2)在此重大事件发生之前,现有的旧系统遭到破坏,而新的但较弱的系统形成了。对于纵向电流螺旋度也确定了类似的变化。 (3)源场在耀斑爆发之前减弱,自由磁能的密度在光球层下降。这些明显的变化持续到“巴士底日”爆发前至少九小时,并且发生在大量的磁通量消失的情况下。还发现剧烈变化的位置与在3D无力重建中看到的螺旋形磁绳的底部重合。我们建议观察到的磁非势的演化表示从低层大气到日冕的磁能和复杂性的连续传输。这种运输似乎是主要火炬能量积累的原因。此外,在低层大气中缓慢的磁重新连接(被视为磁通抵消)似乎在该能量积累过程中起着关键作用。

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  • 来源
    《Solar Physics》 |2001年第2期|11-26|共16页
  • 作者单位

    National Astronomical Observatories Chinese Academy of Sciences;

    National Astronomical Observatories Chinese Academy of Sciences;

    National Astronomical Observatories Chinese Academy of Sciences;

    National Astronomical Observatories Chinese Academy of Sciences;

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  • 正文语种 eng
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