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Statistical characteristics of parameters of sporadic formations in the ionospheric E-region over East Siberia

机译:西伯利亚东部电离层E区零星地层参数的统计特征

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摘要

Presented are the results of a statistical analysis of the ionospheric sounding data over Irkutsk for 1960-1996. It is shown that sporadic features of type "c" and "f" constitute a stationary process. That is, the lower part of the ionospheric E-region that includes the meteor zone develops a region in which the electron density and its variations are governed by two factors, the interaction or dominant influence of one of which leads to sporadic features of one type and to the decay of the other type. The former, steadily acting type is the prevailing wind regime of this ionospheric region, and the other type is the solar control having a predominant influence in summer. Also, the vertical structure of the horizontal wind has effect not on the formation of type "c" E_s but on its decay for the formation of type "1" E_s. Year-to-year variability of the dynamic wind regime dos not affect the number of type "c" E_s features and its frequency parameters.
机译:呈现的是对伊尔库茨克1960-1996年电离层探测数据的统计分析结果。结果表明,类型为“ c”和“ f”的零星特征构成了固定过程。即,包括流星区的电离层E区的下部形成了一个区域,在该区域中,电子密度及其变化受两个因素控制,其中之一的相互作用或显性影响导致一种类型的零星特征和其他类型的衰变。前一种稳定作用类型是该电离层地区的主要风况,另一种类型是在夏季对太阳影响最大的太阳控制。而且,水平风的垂直结构不影响类型“ c” E_s的形成,而是影响其衰减以形成类型“ 1” E_s。动态风况的逐年变化不影响类型“ c”的E_s特征及其频率参数。

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