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Correlative study of plasma bubbles, evening equatorial ionization anomaly, and equatorial prereversal E × B drifts at solar maximum

机译:等离子体气泡,赤道傍晚电离异常和赤道反转E×B在太阳最大时漂移的相关性研究

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摘要

Previous ground observations have revealed a correlation that exists between equatorial plasma bubbles, evening equatorial ionization anomaly (EIA), and prereversal E x B drift velocity using latitudinal arrays of ionospheric sounders, such as in the Indian and American regions. Besides the ground measurements, the space-based observations also provide a convenient way to study the global-scale variations. On the basis of in situ data collected from DMSP, ROCSAT-1, and CHAMP satellites, we investigated the correlation of seasonal/longitudinal variations of plasma bubble (PB) occurrence, evening EIA, and prereversal E × B drifts on magnetically quiet days during the solar maximum years (2000-2002). In general, the observational results provide consistent evidences that the large-scale variations in seasonal/longitudinal distribution of evening EIA and PB occurrence rates are well-correlated with the observed evening prereversal E × B drifts and that some of the small-scale longitudinal variations (such as wave number-4 structure during equinox) of evening EIA exist before the occurrence of the prereversal enhancement and coincide with the daytime equatorial electrojet. In such cases, the small-scale longitudinal variation of PB occurrence rates may result from the evening EIA small-scale longitudinal structures. The evening prereversal E × B drifts, together with the longitudinal variations of evening EIA, are assumed to play a role in determining the longitudinal variations of equatorial and low-latitude PB occurrence rates.
机译:先前的地面观测发现,在印度洋和美洲地区,使用电离层测深仪的纬向阵列,赤道等离子体气泡,赤道傍晚电离异常(EIA)和逆转E x B漂移速度之间存在相关性。除了地面测量外,空基观测还提供了一种方便的方法来研究全球尺度的变化。基于从DMSP,ROCSAT-1和CHAMP卫星收集的原位数据,我们研究了在电磁静天期间血浆气泡(PB)发生,夜间EIA和反转E×B漂移的季节性/纵向变化的相关性。太阳最高年份(2000-2002年)。一般而言,观测结果提供了一致的证据,表明夜间EIA和PB发生率的季节性/纵向分布的大范围变化与观测到的夜间反转E×B漂移和某些小规模的纵向变化密切相关。夜间EIA(例如春分时的4号波结构)在逆转前增强之前就已存在,并且与白天的赤道电喷相吻合。在这种情况下,PB发生率的小规模纵向变化可能是由傍晚的EIA小规模纵向结构引起的。假定夜间反转E×B漂移与夜间EIA的纵向变化一起在确定赤道和低纬PB发生率的纵向变化中起作用。

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