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首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Comparison of quiet time vertical plasma drifts with global empirical models over the Indian sector: Some insights
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Comparison of quiet time vertical plasma drifts with global empirical models over the Indian sector: Some insights

机译:安静时间垂直等离子体与印度部门的全球实证模型的比较:一些见解

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Abstract The threshold vertical plasma drifts and their polarities are inferred from E-region irregularities reported earlier using different experiments conducted from India during geomagnetically quiet time. In addition, the hourly variations of magnetometer data sets are used in conjunction with an equatorial electrojet model (Anandarao, 1976) to deduce the vertical drifts around noon time (10:00–140:00 LT). These results are then compared with the vertical drifts presented by empirical models (Scherliess and Fejer, 1999; Fejer et al., 2008a) corresponding to the 60 ° E longitude sector. In general, the vertical drifts presented by empirical models are consistent with those inferred from snapshot measurements of E-region irregularities at different local times of the day except around sunrise hours. Further, the vertical drifts presented by Fejer et al. (2008a) model match fairly well with seasonally averaged vertical drifts deduced (within 1 σ variation) using magnetometer data. A time difference is noticed between occurrence of pre-reversal enhancement in vertica
机译:<![cdata [ 抽象 从早期报告的电子区域使用从地磁安静时间进行的不同实验推断出阈值垂直等离子体漂移及其极性。此外,磁力计数据集的每小时变化与赤道电气喷射模型(Anandarao,1976)结合使用,以推导中午时间周围的垂直漂移(10:00-140:00 lt )。然后将这些结果与经过经验模型(Scherliess和Fejer,1999; Fejer等,2008a)对应于 60 ° E 经度扇区。通常,经过经验模型所呈现的垂直漂移与除了日出时期之外的不同当前的当前当前的不同当前时期的E区违规的快照测量的垂直漂移是一致的。此外,Fejer等人呈现的垂直漂移。 (2008A)模型与季节性平均垂直漂移相当匹配(在 1 σ 变化)使用磁力计数据。在Vertica中发生逆转增强之间的发生之间注意到时差

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