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摘要: 基于俄罗斯科学院IZMIRAN研究所提供的1998年至2020年期间的电离层总电子含量(TEC)、F2层临界频率(foF2)与峰值高度(hmF2)数据,分析了在地磁活动平静期间经度120°E上空电离层赤道异常(EIA)半球不对称性与冬季纬度位置偏移现象,并探讨其可能影响机制。研究结果表明:夏冬至期间EIA双峰强度不对称性随太阳活动变化特征差异明显,冬至期间不对称性与太阳活动相关性明显,太阳活动低时整体表现为南驼峰较强,太阳活动高时变为以北驼峰较强为主,而夏至期间不对称性与太阳活动变化相关性不显著且趋势与冬至相反;EIA双峰结构纬度位置在冬季期间呈现出向南半球偏移的现象,且南驼峰纬度位置偏移量相对更明显,特别是在太阳活动低时双峰结构偏移特征表现更加显著。在120°E上冬至期间,跨赤道中性风是EIA双峰强度影响半球不对称性的主要因素,在此基础上,冬季EIA双峰结构纬度偏移的主要因素可能与太阳直射点等离子体浓度背景场的地理控制作用有关。Abstract:
In this study, we focus on the morphological features of the interhemispheric asymmetry and latitude offset phenomenon of the equatorial ionization anomaly (EIA) at equatorial and low-latitude magnetic regions in winter by statistics of the parameters -TEC and hmF2 around 120°E longitude during 1998-2020. The results showed that: (1) The hemispherical asymmetry features of EIA structure that vary with solar activity are significantly different during the summer and winter solstice. The asymmetry exhibits a significant correlation with the solar activity during winter solstice. However, there is a weak negative correlation during the summer solstice. (2) The latitude position of EIA structure moves southward in winter months and the latitude deviation of southern anomaly crest is more significant, especially during the low solar activity. The hemispherical asymmetry is mainly affected by the trans-equatorial neutral wind field during the winter solstice. On the other hand, photo-ionization can produce more electrons under the subsolar point, and the effect may plays an important role in Southward offset phenomenon of EIA structure in winter around 120°E longitude. -
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