Abstract

Abstract. The classification of X-ray solar flares is performed regarding their effects on the Very Low Frequency (VLF) wave propagation along the Earth-ionosphere waveguide. The changes in propagation are detected from an observed VLF signal phase and amplitude perturbations, taking place during X-ray solar flares. All flare effects chosen for the analysis are recorded by the Absolute Phase and Amplitude Logger (AbsPal), during the summer months of 2004–2007, on the single trace, Skelton (54.72 N, 2.88 W) to Belgrade (44.85 N, 20.38 E) with a distance along the Great Circle Path (GCP) D≈2000 km in length. The observed VLF amplitude and phase perturbations are simulated by the computer program Long-Wavelength Propagation Capability (LWPC), using Wait's model of the lower ionosphere, as determined by two parameters: the sharpness (β in 1/km) and reflection height (H' in km). By varying the values of β and H' so as to match the observed amplitude and phase perturbations, the variation of the D-region electron density height profile Ne(z) was reconstructed, throughout flare duration. The procedure is illustrated as applied to a series of flares, from class C to M5 (5×10−5 W/m2 at 0.1–0.8 nm), each giving rise to a different time development of signal perturbation. The corresponding change in electron density from the unperturbed value at the unperturbed reflection height, i.e. Ne(74 km)=2.16×108 m−3 to the value induced by an M5 class flare, up to Ne(74 km)=4×1010 m−3 is obtained. The β parameter is found to range from 0.30–0.49 1/km and the reflection height H' to vary from 74–63 km. The changes in Ne(z) during the flares, within height range z=60 to 90 km are determined, as well.

Highlights

  • The lower boundary of the D-region is known, as well as the upper edge of Earth-ionosphere waveguide, for very low frequency (VLF) wave propagation

  • The observed VLF amplitude and phase perturbations are simulated by the computer program Long-Wavelength Propagation Capability (LWPC), using Wait’s model of the lower ionosphere, as determined by two parameters: the sharpness (β in 1/km) and reflection height (H in km)

  • These changes in electron density profile are of crucial importance for the Earth-ionosphere VLF propagation path

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Summary

Introduction

The lower boundary of the D-region is known, as well as the upper edge of Earth-ionosphere waveguide, for very low frequency (VLF) wave propagation. Enhanced D-region density causes the change in the electrical conductivity at the upper waveguide edge along the trace of the VLF signal and gives rise to the change in all propagating parameters These changes are clearly detected as the perturbation of phase and amplitude on the records of the diurnal VLF signal variation. The stable daytime propagation on the GQD path is illustrated by the AbsPAL records on the quiet day of 8 July 2005, shown in Fig. 1; the phase and amplitude measurements (upper and lower plot, respectively) are represented by solid lines. Under regular conditions, stable daytime propagation allows the waveguide to be characterized by a single well-defined (βq =0.30 1/km, Hq =74.0 km) pair These characteristics are given by the GOES 12 X-ray data lists in the wavelength range 0.1–0.8 nm, which can be retrieved via the web site www.sec.noaa.gov

Determination of β and H under flare conditions
Analysis of VLF measurements and calculations results
13 July 2004
Discussion
Conclusion
Full Text
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