首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Variations in Cosmic Noise Absorption in Association With Equatorward Development of the Pulsating Auroral Patch: A Case Study to Estimate the Energy Spectra of Auroral Precipitating Electrons
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Variations in Cosmic Noise Absorption in Association With Equatorward Development of the Pulsating Auroral Patch: A Case Study to Estimate the Energy Spectra of Auroral Precipitating Electrons

机译:宇宙噪声吸收的变化与朝赤道方向发展脉动极光补丁:一个案例研究来评估极光沉淀的能量谱电子

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This study focused on a pulsating aurora event associated with aurora morphological changes in Fennoscandia in the early morning on March 7, 2017. A high-speed sampling all-sky camera captured equatorward development of the pulsating auroral patch in association with a substorm centered over the Greenland/North America region. Of particular interest in this event is the interconnection between the auroral intensity and the cosmic noise absorption (CNA) derived from three riometers aligned meridionally in Finland (from north to south: Ivalo, Sodankyl?, and Rovaniemi). The analysis was made by dividing optical measurements into two oscillation components: longer and shorter than 40 s, that is, nonpulsating and pulsating auroral modulations. The interrelation between the auroral brightness and CNA showed a linear correlation. The inclination of the regression line changed with time depending on latitudes, which was interpreted as hardening or softening of the precipitating electron spectrum. Especially in the case of the low-pass component, the inclination of the CNA-vs-intensity interrelation increased at the three riometer latitudes in the substorm recovery phase. On the other hand, for the high-pass component, the inclination decreased at Rovaniemi (lower latitude) but remained uniform at Sodankyl? (higher latitude). These features suggest that the precipitating electron spectrum has softened in the low-pass or nonpulsating auroral component, but the spectrum has hardened in the high-pass or pulsating auroral component on the lower latitude part of the auroral patch region. This study proposes a new application of riometer-camera measurements to examine auroral particle precipitation.
机译:这项研究集中在一个脉动极光事件与极光形态变化有关Fennoscandia清晨3月7日,2017. 捕获朝赤道方向发展的脉动极光补丁与亚暴集中在格陵兰和北美地区。这个事件是特别感兴趣极光强度和之间的互连(中央社)来源于宇宙噪声吸收三个宇宙噪声测量器在芬兰子午相一致(从北到南:Ivalo Sodankyl吗?罗凡尼米)。光学测量为两个振荡组件:比40年代,长和短是,nonpulsating和脉动极光调节。极光的亮度和CNA显示线性的相关性。随着时间的推移而改变取决于纬度,这被解读为硬化或软化沉淀的电子光谱。特别是在低通组件的情况下,CNA-vs-intensity的倾向在三个宇宙噪声测量器相互关系增加纬度的亚暴复苏阶段。另一方面,对于高通组件,罗凡尼米倾向减少(降低纬度),但仍在Sodankyl制服吗?(更高的纬度)。沉淀的电子光谱软化了在低通或nonpulsating极光组件,但光谱已经变硬高通或脉动极光组件较低的纬度地区极光补丁的一部分。本研究提出了一个新的应用程序riometer-camera测量检查极光粒子沉淀。

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