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A method of estimating horizontal vectors of ionospheric electric field deduced from HF Doppler data

机译:一种从高频多普勒数据推导出的电离层电场水平矢量的估算方法

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摘要

A formulation providing time variations of the horizontal electric field in the ionosphere from HF Doppler data is presented. The relationship between the electric field and frequency deviations of ionospherically reflected HF radio waves has been extended from the theory given by Jacobs and Watanabe in 1966. In the present formula, the effect of electron decay due to attachment and/or recombination processes is taken into account for long-lasting variations in the electric field. The developed formula can provide time variations of the horizontal field vector even from data observed at only one station. The formula has been applied to an isolated substorm event. In examining the validity of the deduced results, equivalent ionospheric current systems have been used. These have been deduced from worldwide magnetometer data. With these current systems, we can roughly estimate the horizontal electric field in the ionosphere under some assumptions. The time variation of the electric field deduced from the HF Doppler data agrees with that deduced from current systems and high latitude electrojet activity. The results indicate that the HF Doppler method is a sensitive and useful tool for estimating the electric field in the ionosphere.
机译:提出了根据HF多普勒数据提供电离层中水平电场随时间变化的公式。电离层反射的HF无线电波的电场与频率偏差之间的关系已从Jacobs和Watanabe于1966年给出的理论中得到了扩展。导致了电场的长期变化。即使仅从一个站观测到的数据,开发的公式也可以提供水平场矢量的时间变化。该公式已应用于孤立的亚暴事件。在检查推论结果的有效性时,使用了等效的电离层电流系统。这些是从全球磁力计数据推论得出的。使用这些电流系统,在某些假设下,我们可以大致估算电离层中的水平电场。从HF多普勒数据推导出的电场时间变化与从当前系统和高纬度电喷活动推导的时间变化一致。结果表明,高频多普勒方法是一种灵敏且有用的工具,用于估算电离层中的电场。

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