Abstract

Solar flare effects (Sfe) are rapid variations in the Earth’s magnetic field and are related to the enhancement of the amount of radiation produced during Solar flare events. They mainly appear in the Earth’s sunlit hemisphere at the same time as the flare observation and have a crochet-like shape. Much progress has been made since Carrington’s first observations in 1859 which are considered to represent the first direct evidence of the connection between the Sun and the Earth’s environment but there is still much to discover. In this paper, we review state-of-the-art developments and the advances made in the knowledge concerning Sfe phenomena while also looking at the challenges that lie ahead. First, we offer a historical approach with a comprehensive description that allows for a better understanding of the main characteristics of Sfe. This frames specific topics like the puzzling reversed-Sfe or the nighttime Sfe. The role played by the Service of Rapid Magnetic variations (SRMV) is also assessed, followed by a discussion of the main current limiting factors in the process of detection and proposed ways to overcome challenges such as by creating an automatic detection method. The paper clarifies some aspects related to the geo-effectiveness of the solar flares producing magnetic disturbances. The importance of the global modelling studies covering critical aspects needed to understand this Sun–Earth system is assessed. Also, we provide an overview of the temporal evolution of the electric currents producing Sfe. The importance of key subjects such as the dynamic aspects of Sfe is developed in another section. Finally, estimations of the size of large flares using ionospheric and magnetic data are reviewed as well as the prospects of these large flare events putting technological systems in danger.

Highlights

  • Solar flare effects (Sfe) are rapid variations in the Earth’s magnetic field and are related to the enhancement of the amount of radiation produced during Solar flare events

  • Van Zele & Meza (2011) undertook the task of evaluating the efficiency of geomagnetic solar flare effects in X-ray solar flare detection. They concluded that the identification of solar flares using Sfe is affected by: the intensity and average growth rate of solar flare radiation – the quicker it is, the more the solar flare is detected as Sfe; the position of the geomagnetic observatory, as observatories placed in the summer hemisphere identify the solar flare more so the uneven geographical distribution of observatories makes solar flare identification difficult; the existing geomagnetic perturbation previous to a solar flare; and the likeness between the Sfe and other geomagnetic variations

  • We present a comprehensive review of the current status of Sfe research

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Summary

Discovery of Sfe

The first time a geomagnetic variation was observed as a result of a solar flare was during the course of the great solar event of September 1, 1859. The types of geomagnetic effects of solar flares and their relationship with the Sq field (Solar quiet = diurnal geomagnetic variation on the days of least magnetic activity; Matsushita & Campbell, 1967) were examined by Imamiti (1938, 1940) at different observatories The results of this test reaffirmed McNish’s conclusion. They found that the predominant increase in ionization in these cases occurred below 100 km and extended to the E-region They concluded that it must be there that the geomagnetic effects and simultaneous ionospheric effects observed were caused. After his direct measurements of solar radiation in space vehicles, that the main ionizing agent of the effects of solar flare was X-rays with wavelengths between 1 and 100 Å

First global studies
Transients in the development of the Sfe
Sfe and solar flares
Sfe and equatorial electrojet
Sfe and micro-pulsations
Night Sfe
General characteristics
Reversed Sfe
History of the service
IAGA bulletins
Likely
The origin of the Sfe lists
Difficulties in Sfe detection
Automatic detection
Past studies
Recent studies
Dynamic aspects
Revisiting large historical flares
Findings
Conclusions
Full Text
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