Unusual nighttime impulsive foF2 enhancements at low latitudes: Phenomenology and possible explanations |
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Authors: | L Perna M Pezzopane E Zuccheretti PR Fagundes R de Jesus MA Cabrera RG Ezquer |
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Institution: | 1. Dipartimento di Fisica, Università di Roma “La Sapienza”, 00185 Rome, Italy;2. Istituto Nazionale di Geofisica e Vulcanologia, 00143 Rome, Italy;3. Universidade do Vale do Paraíba, 12244-000 São José dos Campos, Brazil;4. Laboratorio de Telecomunicaciones, DEEC, FACET, Universidad Nacional de Tucumán, 4000 Tucumán, Argentina;5. Laboratorio de Ionósfera, Departamento de Física, FACET, Universidad Nacional de Tucumán, 4000 Tucumán, Argentina;6. CIASUR, Facultad Regional Tucumán, Universidad Tecnológica Nacional, 4000 Tucumán, Argentina;g Consejo Nacional de Investigaciones Científicas y Técnicas, 1033 Buenos Aires, Argentina |
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Abstract: | This paper is focused on unusual nighttime impulsive electron density enhancements that are rarely observed at low latitudes on a wide region of South America, under quiet and medium/high geomagnetic conditions. The phenomenon under investigation is very peculiar because besides being of brief duration, it is characterized by a pronounced compression of the ionosphere. The phenomenon was studied and analyzed using both the F2 layer critical frequency (foF2) and the virtual height of the base of the F region (h′F) values recorded at five ionospheric stations widely distributed in space, namely: Jicamarca (−12.0°, −76.8°, magnetic latitude −2.0°), Peru; Sao Luis (−2.6°, −44.2°, magnetic latitude +6.2°), Cachoeira Paulista (−22.4°, −44.6°, magnetic latitude −13.4°), and São José dos Campos (−23.2°, −45.9°, magnetic latitude −14.1°), Brazil; Tucumán (−26.9°, −65.4°, magnetic latitude −16.8°), Argentina. In a more restricted region over Tucumán, the phenomenon was also investigated by the total electron content (TEC) maps computed by using measurements from 12 GPS receivers. A detailed analysis of isoheight ionosonde plots suggests that traveling ionospheric disturbances (TIDs) caused by gravity wave (GW) propagation could play a significant role in causing the phenomenon both for quiet and for medium/high geomagnetic activity; in the latter case however a recharging of the fountain effect, due to electric fields penetrating from the magnetosphere, joins the TID propagation and plays an as much significant role in causing impulsive electron density enhancements. |
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Keywords: | Equatorial ionosphere Electron density enhancement Traveling ionospheric disturbance Fountain effect TEC |
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