Ionosphere vertical section modeling and parameter inversion method

Abstract

The invention discloses an ionosphere vertical section modeling and parameter inversion method. The method comprises the following steps: 1, modeling an ionosphere into a four-layer model including an E layer, a valley layer, an F<1> layer and an F<2> layer; 2, deducing a calculation formula of an echo virtual height of each layer based on the established ionosphere model; and 3, performing inversion of an ionosphere parameter of each layer by using measured ionogram data in combination with a calculation result of the echo virtual height of each layer. The ionosphere vertical section modeling and parameter inversion method disclosed by the invention is based on a vertical exploration ionogram inversion method for optimizing F<1> layer parameters and F<2> layer parameters on the basis of the constraint of a shifted Chebyshev polynomial model, namely, echo tracing data in a high region in the F<1> layer are selected after a valley parameter is obtained, and an F<1> layer section polynomial coefficient is calculated under the condition of ensuring continuously smooth constraint of the section. The method is suitable for effectively improving the inversion accuracy and stability under the situation that the F<1> layer is not developed fully.

Description

technical field [0001] The invention relates to the field of ionosphere research and application, in particular to an ionosphere vertical profile modeling and parameter inversion method. Background technique [0002] Ionospheric vertical detection (referred to as vertical measurement) can obtain vertical measurement ionograms that reflect the relationship between the false height and frequency of the ionosphere. The so-called false height is essentially a measure of the propagation time of electromagnetic waves. The time elapsed after arriving at the vertical survey receiver multiplied by the speed of light is called false height. The false height obtained by the vertical survey is not the real reflection height of the electromagnetic wave in the ionosphere, and the acquisition of the real reflection height requires the inversion of the vertical survey ionogram, that is, the inversion of the ionospheric profile by using the vertical survey ionogram frequency-false height tra...

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Problems solved by technology

[0003] At present, the commonly used vertical ionogram inversion method is the ionospheric parameter inversion method based on the idea of ​​the model method. Among them, Huang Xueqin et al. disclosed a method for inverting the ionospheric profile based on the shifted Chebyshev polynomial model , in this method, the F layer is modeled as a shifted Chebyshev polynomial, and the polynomial coefficients that satisfy the best agreement between the calculated virtual height and the measured virtual height in the sense of least squares are solved to determine the ionospheric profile. F is evident in the wave trace 1 In the case of layer tracing, some improvements have been made on the model, that is, F 1 layers and F 2 Layers are represented by different shifted Chebyshev polynomials, but this method is more suitable for F 1 When the layer is fully developed, for F 1 When the layer is not fully developed, the vertical ionogram synthesized based on the inversion results and the measured ionogram are at F 1 There is a large difference near the adjacent frequency of the layer. In addition, the smoothness of the layer-to-layer connection is not considered, which is also the shortcoming of this method.

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