Modelling of the electron density profile in the lowest part of ionosphere D-region on the basis of radiowave absorption data: 1. Theoretical model

Pl. Mukhtarov, D. Pancheva
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引用次数: 3

Abstract

A simplified full-wave method adapted to the propagation of very obliquely incident LF radio waves is developed. For a selected ionosphere model the wave-field structure is calculated inside a horizontally stratified ionosphere and the peculiarities of the reflected field are clearly described. The penetration of the investigated radio waves in the lower ionosphere at noon-time is found to be restricted to a layer several wavelengths thick. The reflected wave is created entirely by the mechanism of partial reflections and the region responsible for its formation is usually below 70 km. The influence of some typical parameters of the electron density profile, as well as the atmospheric pressure and temperature, on the attenuation of the investigated radio waves is demonstrated. It is also found that the reflection at very oblique incidence depends mainly on the height of the bottom of the ionosphere.

基于无线电波吸收数据的电离层d区最低部分电子密度分布模拟:理论模型
提出了一种适用于极斜入射低频无线电波传播的简化全波方法。对于选定的电离层模型,计算了水平分层电离层内的波场结构,并清楚地描述了反射场的特性。所研究的无线电波在正午时分在较低电离层的穿透被发现被限制在几个波长厚的层内。反射波完全由部分反射机制产生,其形成区域通常在70公里以下。论证了电子密度分布的一些典型参数以及大气压力和温度对所研究无线电波衰减的影响。我们还发现,极斜入射时的反射主要取决于电离层底部的高度。
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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