Please use this identifier to cite or link to this item: http://library.iigm.res.in:8080/xmlui/handle/123456798/182
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dc.rights.licenseCC BY
dc.contributor.authorRufai, Odutayo R.
dc.contributor.authorKhazanov, George V.
dc.contributor.authorSingh, S.V.
dc.date.accessioned2022-07-13T04:55:30Z
dc.date.available2022-07-13T04:55:30Z
dc.date.issued2021
dc.identifier.citationResults in Physics, v. 24, https://doi.org/10.1016/j.rinp.2021.104041en_US
dc.identifier.urihttp://library.iigm.res.in:8080/xmlui/handle/123456798/182
dc.description.abstractThe electron-acoustic solitons are studied with two temperature electrons (a hot trapped having vortex-like velocity distribution and a warm adiabatic fluid) and stationary ions. The theoretical model is based on the observations of a mixture of the hot, tenuous magnetospheric and warm, dense magnetosheath plasma particles associated with the asymmetric magnetic reconnection at the Earth’s magnetopause by Magnetospheric Multiscale (MMS). Using the reductive perturbation technique, the model supports the existence of nonlinear electron-acoustic structures derived from the mKdV-like equation. The electron-acoustic waves propagate at supersonic speeds above the electron sound speed. The results are applied to observations of electric field structures in the electron diffusion region (EDR).en_US
dc.language.isoenen_US
dc.subjectMMS observationsen_US
dc.subjectKinetic vortex-like velocity distributionen_US
dc.subjectAdiabatic fluiden_US
dc.subjectElectron-acoustic wavesen_US
dc.subjectReductive perturbation techniqueen_US
dc.subjectAymmetric ESWsen_US
dc.subjectElectron diffusion region (EDR)en_US
dc.subjectEarth’s magnetopauseen_US
dc.titleFinite amplitude electron-acoustic waves in the electron diffusion regionen_US
dc.typeArticleen_US
dcterms.sourcehttps://doi.org/10.1016/j.rinp.2021.104041
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