选择在高纬度地区使用的电离层模型

O. Maltseva
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引用次数: 1

摘要

近年来,人们对电离层高纬带的兴趣日益增加,特别是提出了几个专门的卫星实验来研究电离层高纬带。设定电离层条件的一种形式是使用经验模型。最近,除了传统上使用的IRI模型外,还开发了SIMP和E-CHAIM模型,目的是改进这一特定领域参数的设置。本文采用4种模式(1)IRI2016模式、2)SIMP模式、3)E-CHAIM模式、4)结合2010-2014年朗伊尔城站TEC(obs)观测值和等效电离层板厚τ(med)中值,比较了观测临界频率foF2(obs)与模式频率。此外,通过与SIMP和E-CHAIM模式的对比,补充了IRI2016模式与俄罗斯其他台站试验数据的对比结果。特别注意扰动条件。在这些情况下,建议使用总电子含量TEC。foF2模型值与实验中位数的比较表明,IRI模型和SIMP模型没有优势,E-CHAIM模型提供了1.5倍的最佳拟合:IRI模型的5年平均绝对偏差为0.49 MHz, SIMP模型为0.52 MHz, E-CHAIM模型为0.31 MHz。相对偏差分别为13.36%、13.88%和8.42%。E-CHAIM模型在干扰期间获得foF2具有更大的优势:它反映了白天的正干扰和负干扰,夜间电离增强。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Choice of a model of the ionosphere to use in high latitudes
Recently, interest in the high-latitudinal zone of the ionosphere has increased, in particular, several special satellite experiments have been proposed for studying this zone. One of the forms for setting the conditions of the ionosphere is the use of empirical models. Recently, SIMP and E-CHAIM models have been developed, aimed at improving the setting of parameters in this particular area, in addition to the traditionally used IRI model. In this paper, we compare the observational critical frequencies foF2(obs) with the model frequencies in accordance with 4 options: 1) model IRI2016, 2) model SIMP, 3) model E-CHAIM, 4) join usage of observational values of TEC(obs) and the median of the equivalent ionospheric slab thickness τ(med) according to Longyearbyen station in 2010-2014. In addition, the previous results of the IRI2016 model comparison with experiment according to data from other Russian stations are complemented by a comparison with the SIMP and E-CHAIM models. Special attention is paid to disturbed conditions. It is proposed to use in these cases the total electron content TEC. Comparison of the model values of foF2 and experimental medians showed that the IRI and SIMP models do not have advantages against each other, the E-CHAIM model provides 1.5 times the best fit: the average absolute deviations for 5 years were 0.49 MHz for the IRI model, 0.52 MHz for the SIMP model and 0.31 MHz for the E-CHAIM model. The relative deviations were 13.36%, 13.88% and 8.42%, respectively. The E-CHAIM model has an even greater advantage in obtaining foF2 during disturbances: it reflects positive and negative daytime disturbances, nightly enhancements of ionization.
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