Case study of the ionospheric irregularities in China low latitude during the geomagnetic storm in July 13-14, 2013
-
摘要: 本文研究了2013年7月13日至14日一次中等强度磁暴期间在中国低纬地区发生的电离层不均匀体事件。通常情况下,在北半球夏季,东亚扇区低纬电离层不均匀体不易产生,但此次磁暴期间观测到了显著的不均匀结构增强现象。利用中国地壳运动观测网(CMONOC)和香港卫星定位参考台站网(SatRef)地基GNSS数据、深圳站(22.59°N, 113.97°E)闪烁接收机S4数据、海南富克站(19.4°N, 109.0°E)测高仪数据、以及地磁观测数据等,分析了我国低纬度地区的电离层不均匀体的时空演化过程,并基于磁暴期间的空间环境参量对此次电离层不均匀体的激发机制进行了分析。结果表明,磁暴期间出现的东向电场增强是促进此次电离层不均匀体的发展主要原因。同时,电离层不均匀体出现前测高仪观测到的卫星描迹表明大尺度波状结构可能作为种子作用,为不均匀结构的产生创造了条件。此外,本文还对比了S4指数、ROTI、失锁这几种参量在此次事件中的响应,发现它们在时间分布上大体一致(集中在15:00-18:00 UT),与电离层不均匀体的发生时间一致,但在不均匀结构出现前一个小时出现的L2载波相位失锁(集中在14:00 UT附近)应与本次事件无关。
-
关键词:
- 电离层不均匀体 /
- 电离层闪烁 /
- 磁暴 /
- 总电子含量(TEC) /
- 频高图
Abstract: This study investigates the effects of a moderate geomagnetic storm during July 13-14, 2013 on the development of ionospheric irregularities in the low latitude region of China. Although in the East Asian sector, ionospheric irregularities are relatively uncommon in July, unseasonal irregularities are observed during this geomagnetic storm. Ground-based GNSS data from Crustal Movement Observation Network of China (CMONOC) and Hong Kong Satellite positioning Reference stations (SatRef), S4 index data from the ionospheric scintillation monitor (ISM) at Shenzhen (22.59°N, 113.97°E) station, ionosonde data from Fuke (19.4°N, 109.0°E) station, and geomagnetic data are used in this study to show the evolution of the ionospheric irregularities in the low latitude region of China during the geomagnetic storm. Geomagnetic and solar activity parameters are used to analyze the generation mechanisms of the irregularities. It is shown that the eastward electric field enhanced by the geomagnetic storm is the major factor contributing to the generation of the irregularities. Satellite traces in the ionograms before the onset of the irregularities indicate that large-scale wave structures acting as seed perturbations may also contribute to this event. Furthermore, it is found that the temporal distribution of S4 index and ROTI are generally similar (enhanced during 15:00-18:00 UT) and coincide with the time range of the irregularities, but the distribution of L2 loss of lock is slightly different (occurring around 14:00 UT, about one hour earlier). These loss of lock occurrences are unrelated to this event. -
-
计量
- 文章访问数: 55
- HTML全文浏览量: 3
- PDF下载量: 4
-
被引次数:
0(来源:Crossref)
0(来源:其他)