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dc.contributor.authorLakhina, G.S.
dc.contributor.authorSingh, S.V.
dc.contributor.authorKakad, Amar
dc.contributor.authorGoldstein, M.L.
dc.contributor.authorViñas, A.F.
dc.contributor.authorPickett, J.S.
dc.date.accessioned2015-10-05T09:55:41Z
dc.date.accessioned2021-02-12T09:33:47Z
dc.date.available2015-10-05T09:55:41Z
dc.date.available2021-02-12T09:33:47Z
dc.date.issued2009
dc.identifier.citationJournal of Geophysical Research, v.114, A09212, 2009, doi: 10.029/2009JA014306en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/528
dc.description.abstractElectrostatic solitary waves (ESWs) have been observed in the Earth's magnetosheath region by Cluster. A mechanism for the generation of these structures in terms of electron-acoustic solitons and double layers is discussed. The model simulates the magnetosheath plasma by a four-component plasma system consisting of core electrons, two counterstreaming electron beams, and one type of ions. The analysis is based on the fluid equations and the Poisson equation, and employs the Sagdeev pseudopotential techniques to investigate the solitary waves. The electric field amplitudes, the time durations, and the propagation speeds of the solitary structures predicted by the model are in good agreement with the observed electric fields, pulse widths, and speeds of the electrostatic bipolar pulses.en_US
dc.language.isoenen_US
dc.subjectEarth's magnetosheathen_US
dc.subjectElectrostatic solitary wavesen_US
dc.subjectSolitary wavesen_US
dc.subjectSolitary structuresen_US
dc.titleA mechanism for electrostatic solitary structures in the Earth's magnetosheathen_US
dc.typeArticleen_US
dc.identifier.accession091041
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