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Variations in ionospheric parameters during solar flares

机译:太阳耀斑期间电离层参数的变化

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摘要

Results of studying the ionospheric response to solar flares, obtained based on the incoherent scatter radar observations of the GPS signals and as a result of the model simulations, are presented. The method, based on the effect of partial "shadowing" of the atmosphere by the globe, has been used to analyze the GPS data. This method made it possible to estimate the value of a change in the electron content in the upper ionosphere during the solar flare of July 14, 2000. It has been shown that a flare can cause a decrease in the electron content at heights of the upper ionosphere (h > 300 km) according to the GPS data. Similar effects in the formation of a negative disturbance in the ionospheric F region were also observed during the solar flares of May 21 and 23, 1967, at the Arecibo incoherent scatter radar. The mechanism by which negative disturbances are formed in the upper ionosphere during solar flares has been studied based on the theoretical model of the ionosphere-plasmasphere coupling. It has been shown that an intense ejection of O^sup +^ ions into the above located plasmasphere under the action of a sharp increase in the ion production rate and the thermal expansion of the ionospheric plasma cause the formation of a negative disturbance in the electron concentration in the upper ionosphere. [PUBLICATION ABSTRACT]
机译:提出了研究电离层对太阳耀斑的响应的结果,该结果是基于GPS信号的非相干散射雷达观测结果以及模型仿真的结果而获得的。该方法基于地球对大气部分“阴影化”的影响,已被用于分析GPS数据。通过该方法,可以估计2000年7月14日太阳耀斑期间电离层上部电子含量的变化值。研究表明,耀斑会导致上部电离层高度电子含量的降低。电离层(h> 300 km)根据GPS数据。在1967年5月21日至23日的太阳耀斑期间,在Arecibo非相干散射雷达上也观察到了电离层F区形成负扰动的类似影响。基于电离层-等离子层耦合的理论模型,研究了太阳耀斑期间电离层上部形成负扰动的机理。已经表明,在离子产生速率的急剧增加和电离层等离子体的热膨胀的作用下,O sup +离子强烈喷射到上述的等离子层中,从而在电子中形成负干扰。电离层上部的浓度。 [出版物摘要]

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