论文标题
南美的极光报告在卡林顿风暴中
South American auroral reports during the Carrington storm
论文作者
论文摘要
对磁性超级风暴的调查的重要性不仅限于学术兴趣,因为这些超级风暴会由于我们对技术基础设施的依赖性增加,因此会对现代文明产生灾难性影响。在这种情况下,由于极光椭圆形的磁性干扰和赤道范围,1859年9月的卡林顿风暴被认为是观察史的基准。到目前为止,当时最近发表了几份Auroral报告,但这些报告主要来自北半球。在这项研究中,我们分析了来自南美及其附近的数据尿道报告,使用语言学和星体方法评估极光范围,确定在-17.3°磁性纬度和进一步极点的极光可见性,并重建极光椭圆形的赤道边界,即25.1°+/- 0.5°0.5°invariant latitive in varriant latitive。有趣的是,在南美地区,据报道,比北半球更明亮,更丰富多彩的极光表现。与磁性共轭点相比,这种南北不对称性可能与南美的磁性经度变化和较弱的磁场有关,并且磁层电子沉淀到上层大气中的量增加。这些结果证明,卡林顿风暴的大小表明其范围属于其他超级风暴的范围,例如1921年5月和1872年2月在极光椭圆形的赤道边界方面发生的范围。
The importance of the investigation of magnetic superstorms is not limited to academic interest, because these superstorms can cause catastrophic impact on the modern civilisation due to our increasing dependency on technological infrastructure. In this context, the Carrington storm in September 1859 is considered as a benchmark of observational history owing to its magnetic disturbance and equatorial extent of the auroral oval. So far, several recent auroral reports at that time have been published but those reports are mainly derived from the Northern Hemisphere. In this study, we analyse datable auroral reports from South America and its vicinity, assess the auroral extent using philological and astrometric approaches, identify the auroral visibility at - 17.3° magnetic latitude and further poleward and reconstruct the equatorial boundary of the auroral oval to be 25.1° +/- 0.5° in invariant latitude. Interestingly, brighter and more colourful auroral displays were reported in the South American sector than in the Northern Hemisphere. This north-south asymmetry is presumably associated with variations of their magnetic longitude and the weaker magnetic field over South America compared to the magnetic conjugate point and the increased amount of magnetospheric electron precipitation into the upper atmosphere. These results attest that the magnitude of the Carrington storm indicates that its extent falls within the range of other superstorms, such as those that occurred in May 1921 and February 1872, in terms of the equatorial boundary of the auroral oval.