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Long-term Spatial and Temporal Variations of Aurora Borealis Events in the Period 1700 - 1905

机译:1700年至1905年期间北极光事件的长期时空变化

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Catalogues and other records of aurora-borealis events were used to study the long-term spatial and temporal variation of these phenomena in the period from 1700 to 1905 in the Northern Hemisphere. For this purpose, geographic and geomagnetic coordinates were assigned to approximately 27 000 auroral events with more than 80 000 observations. They were analyzed separately in three large-scale areas: i) Europe and North Africa, ii) North America, and iii) Asia. There was a clear need to fill some gaps existing in the records so as to have a reliable proxy of solar activity, especially during the 18th century. In order to enhance the long-term variability, an 11-year smoothing window was applied to the data. Variations in the cumulative numbers of auroral events with latitude (in both geographic and geomagnetic coordinates) were used to discriminate between the two main solar sources: coronal mass ejections and high-speed streams from coronal holes. The characteristics of the associated auroras correlate differently with the solar-activity cycle.
机译:北半球极光事件的目录和其他记录用于研究北半球1700年至1905年期间这些现象的长期时空变化。为此,将地理和地磁坐标分配给了约27 000个极光事件,并进行了80 000多个观测。在三个大型区域分别对它们进行了分析:i)欧洲和北非,ii)北美和iii)亚洲。显然有必要填补记录中存在的一些空白,以便获得太阳活动的可靠代表,尤其是在18世纪。为了增强长期可变性,将11年的平滑窗口应用于数据。极光事件累积数随纬度的变化(在地理坐标和地磁坐标中)被用来区分两种主要的太阳能源:日冕物质抛射和日冕洞的高速流。相关极光的特征与太阳活动周期有不同的相关性。

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