Abstract
In this study we investigated the effects of ionosphere on variations of Total Electron Content (TEC), and consequently deviations on regional models of Vertical TEC (VTEC), as well as variations in ionospheric GPS stations was analyzed using PRN 1 and PRN 32 codes. The estimation algorithm is applied to the computed VTEC data for Maidanak GPS station on 24 September 2021.
Highlights
In this study we investigated the effects of ionosphere on variations of Total Electron Content (TEC), and deviations on regional models of Vertical TEC (VTEC), as well as variations in ionospheric Global Positioning System (GPS) stations was analyzed using PRN 1 and PRN 32 codes
The uppermost part of the ionosphere, above the F2 layer is termed the topside of the ionosphere
TEC can provide an overall description of the ionization in the ionosphere, and can be used for practical applications of radio wave propagation
Summary
In this study we investigated the effects of ionosphere on variations of Total Electron Content (TEC), and deviations on regional models of Vertical TEC (VTEC), as well as variations in ionospheric GPS stations was analyzed using PRN 1 and PRN 32 codes. Due to the altitude variations in the atmospheric neutral composition and the INTERNATIONAL SCIENTIFIC DISCUSSION: PROBLEMS, TASKS AND PROSPECTS Production rate with altitude, the plasma density in the ionosphere has a vertical layered structure, denoted by the D, E, and F layers. Each layer is controlled by different physical processes and has different main ions.
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