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The method of TID characteristics reconstruction from simultaneous measurements by oblique incidence and vertical incidence ionosondes

机译:斜入射和垂直入射超声探空仪同时测量的TID特性重建方法

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The radiophysical complex of the Institute of Solar-Terrestrial Physics for ionospheric investigations consists of ionosonde DPS-4 in Irkutsk (52.25N, 104.27E), Irkutsk incoherent scatter radar which is located about 100 km to the north-west from Irkutsk and chirp-ionosonde (its receiving point is located close to Tory settlement about 100 km to the south-west from Irkutsk). On account of its capabilities the complex can be used as diagnostic tool for investigation of travelling ionospheric disturbances (TID). The work is devoted to the method for reconstruction of TID propagation characteristics by means of cross-correlation and spectrum analysis of simultaneous measurements data obtained by vertical incidence ionosonde and oblique incidence chirp-ionosonde. The height electron density profiles for spaced-apart points are used as data for the analysis. The electron density profiles in Irkutsk are reconstructed from the DPS-4 ionogram using the Reinisch and Huang method with the extrapolation above the peak height. The height electron density profiles for oblique incidence path midpoint are reconstructed according to the Reinisch-Huang method (as it is in DPS-4 ionosonde) from height-frequency characteristic (for path midpoint) which calculated through chirp-ionosonde data by means of the modified Smith method. TID propagation characteristics were reconstructed for the 16th of December of 2006 (when was magnetically disturbed day) through electron density obtained by DPS-4 ionosonde in Irkutsk and electron density profiles reconstructed for path midpoints of Norilsk-Tory and Magadan-Tory paths (Fig. 1) from chirp-ionosonde data (in this case the distance between points of triangle is about 1500 km).
机译:太阳电地球研究所用于电离层研究的放射性物理复合体由伊尔库茨克(52.25N,104.27E)的离子探空仪DPS-4,伊尔库茨克非相干散射雷达组成,该雷达位于距伊尔库茨克和线性调频雷达西北约100公里处。 ionosonde(接收点位于距伊尔库茨克西南约100公里的Tory定居点附近)。由于其功能,该综合体可用作诊断工具,用于研究电离层干扰(TID)。这项工作致力于通过互相关和频谱分析来重建TID传播特性的方法,该方法同时分析了垂直入射离子探空仪和斜入射chi离子探空仪获得的同时测量数据。间隔开的点的高度电子密度分布用作分析数据。伊尔库茨克的电子密度分布图是使用Reinisch和Huang方法从DPS-4离子图重建的,外推在峰高以上。根据Reinisch-Huang方法(在DPS-4离子探空仪中),通过chi声波探空仪数据,通过height频离子探空仪数据计算出的高度-频率特性,重建了斜入射路径中点的高度电子密度分布图(在DPS-4离子探空仪中就是这样)。修改的史密斯方法。通过DPS-4离子探空仪在伊尔库茨克获得的电子密度和2006年12月16日(受到电磁干扰的时候)的TID传播特性得到重建,并为Norilsk-Tory和Magadan-Tory路径的路径中点重建了TID传播特性(图7)。 1)来自chi声波探空仪数据(在这种情况下,三角形的点之间的距离约为1500 km)。

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