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dc.contributor.authorSingh, S.V.
dc.contributor.authorLakhina, G.S.
dc.contributor.authorBharuthram, R.
dc.date.accessioned2017-03-07T11:46:59Z
dc.date.accessioned2021-02-12T09:49:00Z-
dc.date.available2017-03-07T11:46:59Z
dc.date.available2021-02-12T09:49:00Z-
dc.date.issued1996
dc.identifier.citationEarth, Moon, and Planets, v.74/3, p.231-242, 1996, doi: 10.1007/BF00055189en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/956-
dc.description.abstractEnergetic protons haying ring type distributions are shown to generate low-frequency electrostatic waves, propagating nearly transverse to the geomagnetic field lines, in the ring current region by exciting Mode 1 arid Mode 2 nonresonant instabilities and a resonant instability. Mode 1 nonresonant instability has frequencies around ~4 Hz with transverse wavelengths of ~(8–80) km, and it is likely to occur in the region L = (7–8). Mode 2 nonresonant instability can generate frequencies ~(850–1450) Hz with transverse wavelengths ~(2–20) km. The typical frequencies and transverse wavelengths associated with the resonant instability are (950–1250) Hz and (30–65) km. Both the Mode 2 nonresonant instability and the resonant instability can occur in the ring current region with L = (4–6). The low-frequency modes driven by energetic protons could attain maximum saturation electric field amplitude varying from 0.8 mV/m to 70 mV/m. It is suggested that the turbulence produced by the low-frequency modes may cause pitch angle scattering of ring current protons in the region outside the plasmapause resulting in the ring current decay.en_US
dc.language.isoenen_US
dc.subjectElectric fielden_US
dc.subjectEnergetic protonsen_US
dc.subjectElectrostatic wavesen_US
dc.titleLow-frequency electric field fluctuations excited by ring current protonsen_US
dc.typeArticleen_US
dc.identifier.accession091280
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