Bulletin of the Russian Academy of Sciences Physics · 2017 · 11 citations · 14 references
Natural SciencesEarth SciencesGeophysicsAtmospheric RadiationGeomagnetismPlasma PhysicsGeomagnetic Field SourcesPlanetary MagnetospheresSpace PlasmasSpace WeatherMagnetospheric Boundary LayersMagnetospheric DynamicsMagnetospheric PlasmaMagnetospheric StructureRadiation Belt DynamicsRadiation Belt EnhancementRadiation Belts
More than 500 X-ray emission events generated by precipitating electrons from the outer radiation belt have been recorded in the Earth’s atmosphere over the many years of the Lebedev Physical Institute observing fluxes of ionized radiation. This precipitation is closely related to high-velocity solar wind streams, whose rate of occurrence, like that of precipitation events, is greatest during the decline phase of the 11-year solar activity cycle. This work considers the relationship between the high-velocity solar wind, the relativistic electron fluxes in the outer radiation belt, and the electron precipitation observed in the polar atmosphere.
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Acceleration and loss of relativistic electrons during geomagnetic storms
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Rapid local acceleration of relativistic radiation-belt electrons by magnetospheric chorus
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Outward radial diffusion driven by losses at magnetopause
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Energetic Particle Influence on the Earth’s Atmosphere
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