An Integral-Equation Approach to ELF Propagation in a Non-Stratified Earth-Ionosphere Waveguide


Book Description

This report develops and applies a practical method for analyzing long-wave propagation under conditions where the properties of the earth-ionosphere waveguide change markedly over lateral distances comparable to a wavelength or Fresnel zone. Full-wave solutions are used to describe both the vertical and horizontal dependences of the fields, but certain compromises are made to achieve tractability. The method is thus characterized as quasi-full-wave. Its main limitation is that the equation describing the vertical dependence is assumed to nearly decouple from the equation governing the lateral dependence. The method is valid at any frequency for which waveguide modes describe terrestrial propagation. Nonetheless, its practical utility is probably limited to ELF because the lateral properties of the earth-ionosphere waveguide are usually gradual enough to permit use of the WKB approximation at higher frequencies. To facilitate numerical solution, the lateral equation is transformed into an integral equation that accounts for most full-wave properties, including diffraction around a localized disturbance and reflection from lateral gradients. Numerical solutions based on model disturbances having lateral gradients in the direction of propagation reveal a standing wave pattern in front of the disturbance.




ELF Propagation in a Non-Stratified Earth-Ionosphere Waveguide


Book Description

This report analyzes extremely low-frequency (ELF) propagation under conditions where the properties of the earth-ionosphere waveguide change markedly over transverse distances comparable with the width of a Fresnel zone. An integral equation formulation is presented that can be used to obtain numerical results for most types of daytime ionospheric disturbances. Approximate solutions are given for ionospheric disturbances of the type that would occur in single-burst nuclear environments. These fullwave results are compared with results calculated from the widely used two-dimensional WKB approximation, which neglects transverse ionospheric gradients. It is shown that this WKB approximation gives good results for burst-heights above about 100 km, but that fullwave theory that accounts for transverse gradients must be used for lower burst altitudes. For these lower burst-heights, the WKB method seriously overstates the propagation anomaly caused by an on-path burst and understates the anomaly caused by an off-path burst. (Author).













Resonances in the Earth-Ionosphere Cavity


Book Description

This book on electromagnetic resonance phenomena describes a general approach to physical problems, ways to solve them, and properties of the solutions obtained. Attention is given to the discussion and interpretation of formal and experimental data and their links to global atmospheric conditions such as the dynamics of global thunderstorm activity, variations of the effective height of the lower ionosphere, etc. Schumann resonance is related to worldwide thunderstorm activity, and simultaneously, to global properties of the lower ionosphere. Transverse resonance is predominantly a local phenomenon containing information on the local height and conductivity of the lower ionosphere and on nearby thunderstorm activity. Transient events in ELF-VLF radio propagation are also treated. These are natural pulsed radio signals and/or abrupt changes of manmade VLF radio signals. The transients associated with cloud-to-ionosphere discharges (red sprites, blue jets, trolls) are discussed, and clarification of the underlying physical ideas and their practical applications to pioneer results achieved in the field recently are emphasised.










ELF Propagation in the Presence of Nonstratified Ionospheric Disturbances


Book Description

This report analyzes the propagation of the TEM-ELF waveguide mode when the ionosphere is not stratified. It treats strong localized ionospheric disturbances by recasting the lateral wave equation as a two-dimensional integral equation, and applies a specially developed algorithm to obtain numerical solutions. The quasi-full-wave results show that a localized ionospheric disturbance behaves like a converging cylindrical lens filling a narrow aperture. Lateral diffraction and focusing, ignored in treatments that do not fully account for transverse ionospheric structure, cause the ELF signal to exhibit a pattern of maxima and minima on the line normal to the path passing through the center of the disturbance. As expected, the focusing/diffraction effects diminish when the transverse dimension of the disturbance exceeds the width of the first Fresnel zone--typically, several megameters. The analysis models widespread inhomogeneities, such as within the polar cap or at the day/night terminator, as semiinfinite regions separated by diffuse boundaries; it then derives full-wave analytic expressions for the reflection of the TEM mode. Mode reflection is found to significantly affect an ELF signal in two actual situations: first, when receivers are on great circle paths that are nearly tangential to the disturbed polar cap--in which case shadow zones and interference patterns can occur; and second, when signals are incident on the day/night terminator (from the day side) at angles exceeding about 75 deg--in which case the signals are affected by a phenomenon analogous to total internal reflection. Reflection is found to be unimportant if the boundary thickness exceeds about one-sixth of a wavelength. (Author).