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dc.contributor.authorRufai, O.R.
dc.contributor.authorBharuthram, R.
dc.contributor.authorSingh, S.V.
dc.contributor.authorLakhina, G.S.
dc.date.accessioned2015-12-01T11:33:02Z
dc.date.accessioned2021-02-12T09:51:38Z-
dc.date.available2015-12-01T11:33:02Z
dc.date.available2021-02-12T09:51:38Z-
dc.date.issued2014
dc.identifier.citationCommunications in Nonlinear Science and Numerical Simulation,v.19/5, p.1338-1346, 2014, doi: 10.1016/j.cnsns.2013.09.024en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/726-
dc.description.abstractProperties of obliquely propagating ion-acoustic solitons and double layers in a magnetized auroral plasma composed of hot adiabatic ions and two types of, cool and hot Maxwellian electrons are studied using Sagdeev pseudo-potential technique and assuming the quasi-neutrality condition. The new and surprising result which emerges from the model is that in contrast to the case of cold ions where ion-acoustic solitons and double layers are found for subsonic Mach numbers only, the hot ions case allows these nonlinear structures to exist for both subsonic and supersonic Mach number regimes. The double layers exist at lower angle of propagation as hot ion temperature is increased. The soliton electric field amplitudes are increased but their width and pulse duration are decreased with the increase in hot ion temperature. For the auroral zone parameters, the maximum electric field amplitude, width, pulse duration and speed for the solitons come out to be in the range ∼ (0.3–15) mV/m, ∼ (195–455) m, (7–20) ms and (22–26) km/s, respectively. The results seem to be in agreement with the Viking satellite observations in the auroral zone.en_US
dc.language.isoenen_US
dc.subjectLow-frequency wavesen_US
dc.subjectMagnetized plasmaen_US
dc.subjectSolitons and double layersen_US
dc.subjectSagdeev pseudopotentialen_US
dc.subjectAdiabatic ions temperatureen_US
dc.subjectCool and hot electronsen_US
dc.subjectMach numbersen_US
dc.subjectAuroral zoneen_US
dc.titleEffect of hot ion temperature on obliquely propagating ion-acoustic solitons and double layers in an auroral plasmaen_US
dc.typeArticleen_US
dc.identifier.accession091390
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