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Precursory Signs of Large Forbush Decreases

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Abstract

The study of space-weather effects and more specifically Forbush decreases of the cosmic-ray intensity depends on space and ground measurements. Very often Forbush decreases and geomagnetic storms are accompanied by pre-increases and/or pre-decreases manifested in cosmic-ray behavior, known as precursory signs. These cosmic-ray intensity variations do not coincide with the shock arrival but begin well before (up to 24 hours) the onset of the main event. In this study a group of large Forbush decreases with amplitude ≥ 4% was examined for precursors. According to the helio-longitude of the solar source, the events were separated into three categories: western (\(21^{\circ} \leq \) helio-longitude ≤ 60), eastern (\(-60^{\circ} \leq \) helio-longitude \(\leq -21^{\circ}\)), and central (\(-20^{\circ} \leq \) helio-longitude \(\leq 20^{\circ}\)). The selected events cover 1967 – 2017. The analysis of the Forbush decreases and the plotting of the asymptotic longitudinal cosmic-ray distribution diagrams were based on the “Global Survey Method” and the “Ring of Stations” method, respectively. Data on solar flares, solar-wind speed, interplanetary magnetic field, and geomagnetic indices (Kp and Dst) were also used. The results show the clear signs of precursors in a significant number of events.

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Acknowledgements

We greatfully acknowledge the contribution of all the neutron-monitor station teams of the NMDB database (www.nmdb.eu) for providing high-resolution cosmic-ray data. The authors from IZMIRAN wish to acknowledge the support of the Russian Science Foundation under grant 20-72-10023. This work is based on the experimental data of the “Russian National Network of Cosmic Ray Stations” (SCR Network). The project ISEST/MiniMax24 (International Study of Earth-affecting Solar Transients) in the VarSITI has partly supported this study.

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Papailiou, M., Abunina, M., Mavromichalaki, H. et al. Precursory Signs of Large Forbush Decreases. Sol Phys 296, 100 (2021). https://doi.org/10.1007/s11207-021-01844-y

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