1859年9月卡灵顿耀斑的星等估计:从原始记录看

H. Hayakawa, S. Bechet, F. Clette, H. Hudson, H. Maehara, K. Namekata, Y. Notsu
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引用次数: 4

摘要

1859年9月的卡灵顿耀斑是一个基准,是最早报道的太阳耀斑,也是对地球影响最大的事件之一。迄今为止,根据唯一可用的直接观测,即它的白光发射,还没有对这一耀斑的能量做出严格的估计。在这里,我们利用历史观测来获得一个星等估计,并将其表示为GOES软x射线类。根据卡灵顿的原始图纸,我们估计白光闪耀区域的面积为116±25米什。卡灵顿的解释允许我们估计耀斑黑体的亮度温度为≈8800-10,900 K,给出了对所报道的耀斑亮度最合理的解释。这导致在现代修订的GOES尺度上,史无前例的分类估计为≈X80 (X46-X126)(比传统的高1.43倍)。这大大超过了先前的估计,但这是基于对卡灵顿描述的明确解释。我们还描述了一种替代的但不太可信的耀斑亮度估计,如以前所采用的,以获得≈X14 (X9-X19)的类估计。这种现在已被弃用的情景给出的估计与直接观测到的现代大耀斑相似。“等效面积”的近似值,基于日野岛的观测,得出了可比较的量级,并批准了我们的估计,尽管有更大的不确定性范围。我们注意到,我们的首选估算值高于目前使用的基于间接地磁测量的X64.4±7.2(修正)。
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Magnitude Estimates for the Carrington Flare in 1859 September: As Seen from the Original Records
The Carrington flare in 1859 September is a benchmark, as the earliest reported solar flare and as an event with one of the greatest terrestrial impacts. To date, no rigorous estimate of the energy of this flare has been made on the basis of the only direct observation available, its white-light emission. Here, we exploit the historical observations to obtain a magnitude estimate and express it in terms of its GOES soft X-ray class. From Carrington’s original drawings, we estimated the area of the white-light flaring region to be 116 ± 25 msh. Carrington’s account allows us to estimate the flare blackbody brightness temperature as ≈8800–10,900 K, given the most plausible interpretation of the reported flare brightness. This leads to an unprecedented class estimate of ≈X80 (X46–X126), on the modern revised GOES scale (a factor 1.43 higher than the traditional one). This substantially exceeds earlier estimates but is based on an explicit interpretation of Carrington’s description. We also describe an alternative but less plausible estimation of the flare brightness, as adopted previously, to obtain a class estimate of ≈X14 (X9–X19). This now-deprecated scenario gives an estimate similar to that of with those of directly observed modern great flares. Approximations with “equivalent area,” based on the Hinode observations, lead to comparable magnitudes and approve our estimates, though with a larger uncertainty range. We note that our preferred estimate is higher than the currently used value of X64.4 ± 7.2 (revised) based on indirect geomagnetic measurements.
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