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Dynamics and structure of the vertical ionospheric disturbances caused by Tohoku earthquake according to Irkutsk bistatic CHIRP-sounding

机译:根据伊尔库茨克双基地CHIRP探测,东北地震引起的垂直电离层扰动的动力学和结构

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In the work we present results of observation of the mid-scale vertical ionospheric irregularities caused by Tohoku earthquake (11/03/2011, 05:47UT) at distance 3400km from epicenter with 1 minute temporary resolution. Their spatial and temporary dynamics is also investigated. As showed the analysis of the experimental data, the main response of the ionosphere was observed at Irkutsk from 06:10UT to 07:00UT. Short-term variations of the electron density profile were also observed from 06:00UT. This corresponds to the main horizontal speed of disturbances about 4, 2–2.5 and 1.2–1.3 km/s. The vertical scale of the irregularities was 10–20 km. Irregularities practically weren't observed at heights above 180200km.
机译:在工作中,我们提出了在距震中3400 km的位置,由东北地震(11/03 / 2011,05:47UT)引起的中尺度垂直电离层不规则现象的观测结果,临时分辨率为1分钟。还研究了它们的空间和暂时动力学。如对实验数据的分析所示,在伊尔库茨克从06:10UT到07:00UT观察到了电离层的主要响应。从06:00UT也观察到电子密度分布的短期变化。这相当于扰动的主要水平速度约为4、2–2.5和1.2–1.3 km / s。不规则的垂直尺度为10–20 km。实际上,在180200 km以上的高度没有观察到不规则性。

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