Some Inexactnesses of the European NeQuick Model and Possible Ways of their Correction

S. Grinchenko
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Abstract

NeQuick model is used in particular in solving problems of radio wave propagation in ionosphere. It allows of calculation of the altitude profiles of electron density above any point of the globe in a wide range of altitudes at any time. The makers of NeQuick model use analytical formulas for the description of the separate E, F1, and F2 layers in constructing of the electron density profile for the whole altitude region. The formula parameters use previously calculated values of electron density and height of the layer peaks. But the insufficient correctness of algorithmization results in some inaccuracies of construction of total profile of electron density in heights of E and F1 regions. For example, there are time discontinuities of daily variations of electron density at the moments corresponding to appearance or disappearance of layer F1. The E and F1 layers practically do not manifest themselves on figures of the electron density profiles. In addition, the previously calculated F1-layer peaks do not lie on the electron density profiles. By means of the algorithm of construction of electron density profile developed by the author of this paper it is possible to describe correctly an altitude profile of electron density on its geometrical parameters of E, F1, and F2 regions. The corrected altitude profiles would change continuously with local time.
欧洲NeQuick模式的一些不精确之处及可能的修正方法
NeQuick模型特别用于求解无线电波在电离层中的传播问题。它允许在任何时间在大范围的高度范围内计算地球上任何一点以上的电子密度的高度分布。NeQuick模型的制作者在构建整个海拔区域的电子密度剖面时,使用解析公式对E、F1和F2层进行描述。公式参数使用先前计算的电子密度值和层峰高度。但由于算法的准确性不足,导致E区和F1区高度电子密度总剖面的构建存在一定的不准确性。例如,在F1层出现或消失的时刻,电子密度的日变化存在时间不连续。E层和F1层实际上在电子密度分布图上并不表现出来。此外,先前计算的f1层峰并不位于电子密度分布图上。本文提出的构造电子密度分布图的算法,可以根据E、F1和F2区域的几何参数,正确地描述电子密度的高度分布图。校正后的高度剖面将随当地时间连续变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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