1990
DOI: 10.1016/0032-0633(90)90154-i
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The ionospheric effects in D-layer and solar proton precipitation zones during the 16 February 1984 event

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Cited by 5 publications
(1 citation statement)
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“…Subsequently, Mendes and Ananthakrishnan [1972] calculated the relative parts of the examined TRGCPs affected by the SPEs (based on two events), as well as the VLF reflection height change (that reached an enormous 23 km in one of the TRGCPs), due to these events. Beloglazov et al [1990] examined a single SPE that occurred during 1984 using VLF NB, riometer, and satellite data, and concluded that the electron density at an altitude of 45 km steeply rose to 1000 km -1 during the event. In addition, they demonstrated the existence of two regions and mechanisms responsible for the ionization produced by the protons; the direct impact zone in the polar cap's center, and the day-evening auroral sector affected by SPE-driven precipitation of quasi-trapped magnetospheric electrons.…”
Section: Solar Proton Eventsmentioning
confidence: 99%
“…Subsequently, Mendes and Ananthakrishnan [1972] calculated the relative parts of the examined TRGCPs affected by the SPEs (based on two events), as well as the VLF reflection height change (that reached an enormous 23 km in one of the TRGCPs), due to these events. Beloglazov et al [1990] examined a single SPE that occurred during 1984 using VLF NB, riometer, and satellite data, and concluded that the electron density at an altitude of 45 km steeply rose to 1000 km -1 during the event. In addition, they demonstrated the existence of two regions and mechanisms responsible for the ionization produced by the protons; the direct impact zone in the polar cap's center, and the day-evening auroral sector affected by SPE-driven precipitation of quasi-trapped magnetospheric electrons.…”
Section: Solar Proton Eventsmentioning
confidence: 99%