Abstract

Abstract. We have investigated the solar flare effects on ionospheric absorption with the systematic analysis of ionograms measured at midlatitude and low-latitude ionosonde stations under different solar zenith angles. The lowest recorded ionosonde echo, the minimum frequency (fmin, a qualitative proxy for the “nondeviative” radio wave absorption occurring in the D-layer), and the dfmin parameter (difference between the value of the fmin and the mean fmin for reference days) have been considered. Data were provided by meridionally distributed ionosonde stations in Europe and South Africa during eight X- and M-class solar flares in solar cycle 23. Total and partial radio fade-out was experienced at every ionospheric station during intense solar flares (> M6). The duration of the total radio fade-out varied between 15 and 150 min and it was highly dependent on the solar zenith angle of the ionospheric stations. Furthermore, a solar-zenith-angle-dependent enhancement of the fmin (2–9 MHz) and dfmin (1–8 MHz) parameters was observed at almost every station. The fmin and dfmin parameters show an increasing trend with the enhancement of the X-ray flux. Based on our results, the dfmin parameter is a good qualitative measure for the relative variation of the “nondeviative” absorption, especially in the case of the less intense solar flares, which do not cause total radio fade-out in the ionosphere (class < M6).

Highlights

  • The most intense external impact on the ionosphere from above is related to solar flares

  • In the present study we investigated the response of ionospheric absorption to solar flares, with particular interest in the solar zenith angle dependence variation of it

  • We examined three parameters that can be determined from ionograms: duration of the total radio fade-out, the value of the fmin parameter and the value of the dfmin parameter

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Summary

Introduction

The most intense external impact on the ionosphere from above is related to solar flares. In addition to electromagnetic radiation, solar flares are accompanied by energetic particles (protons and electrons) with energies from some tens of kiloelectronvolts to some hundreds of megaelectronvolts. They reach the Earth’s atmosphere between a half-hour and a few hours later and cause impact ionization (Rishbeth and Garriot, 1969; Bothmer and Daglis, 2007; Tsurutani et al, 2009). The approximate peak electron energy of a few kiloelectronvolts causes the largest

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