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Authors: | Settimi, A.* Bianchi, S.* |
Title: | Ray theory formulation and ray tracing method. Application in ionospheric propagation | Journal: | quaderni di geofisica | Series/Report no.: | 121/ (2014) | Issue Date: | 23-Oct-2014 | URL: | http://istituto.ingv.it/l-ingv/produzione-scientifica/quaderni-di-geofisica/ | Keywords: | Phase and ray velocity Refractive index surface equation Ray surface equation Phase memory concept Canonical ray equations Application of Hamilton's equations Hamilton’s ray equations with spherical coordinates Fermat’s principle General ray theory for a time-varying medium Ray tracing method |
Subject Classification: | 01. Atmosphere::01.02. Ionosphere::01.02.04. Plasma Physics 01. Atmosphere::01.02. Ionosphere::01.02.05. Wave propagation 05. General::05.01. Computational geophysics::05.01.05. Algorithms and implementation 05. General::05.05. Mathematical geophysics::05.05.99. General or miscellaneous 05. General::05.06. Methods::05.06.99. General or miscellaneous |
Abstract: | This work will lead to ray theory and ray tracing formulation. To deal with this problem the theory of classical geometrical optics is presented, and applications to ionospheric propagation will be described. This provides useful theoretical basis for scientists involved in research on radio propagation in inhomogeneous anisotropic media, especially in a magneto-plasma. Application in high frequencies (HF) radio propagation, radio communication, over-the-horizon-radar (OTHR) coordinate registration and related homing techniques for direction finding of HF wave, all rely on ray tracing computational algorithm. In this theory the formulation of the canonical, or Hamiltonian, equations related to the ray, which allow calculating the wave direction of propagation in a continuous, inhomogeneous and anisotropic medium with minor gradient, will be dealt. At least six Hamilton’s equations will be written both in Cartesian and spherical coordinates in the simplest way. These will be achieved by introducing the refractive surface index equations and the ray surface equations in an appropriate free-dimensional space. By the combination of these equations even the Fermat’s principle will be derived to give more generality to the formulation of ray theory. It will be shown that the canonical equations are dependent on a constant quantity H and the Cartesian coordinates and components of wave vector along the ray path. These quantities respectively indicated as ri(τ), pi(τ) are dependent on the parameter τ, that must increase monotonically along the path. Effectively, the procedure described above is the ray tracing formulation. In ray tracing computational techniques, the most convenient Hamiltonian describing the medium can be adopted, and the simplest way to choose properly H will be discussed. Finally, a system of equations, which can be numerically solved, is generated. |
Appears in Collections: | Article published / in press |
Files in This Item:
File | Description | Size | Format | |
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quaderno121.pdf | Main article | 1.31 MB | Adobe PDF | View/Open |
ACCEPTED Settimi A. and Bianchi S. (2014), Quaderni di Geofisica 121, pp. 21.doc | Accepted Manuscript (Word) | 8.8 MB | Microsoft Word |
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