Ion temperature anisotropy instabilities in planetary magnetosheaths

dc.contributor.authorRemya, B.
dc.contributor.authorReddy, R.V.
dc.contributor.authorTsurutani, B.T.
dc.contributor.authorLakhina, G.S.
dc.contributor.authorEcher, E.
dc.date.accessioned2015-10-27T07:16:33Z
dc.date.accessioned2021-02-12T09:31:57Z
dc.date.available2015-10-27T07:16:33Z
dc.date.available2021-02-12T09:31:57Z
dc.date.issued2013
dc.description.abstractThere has been a lack of understanding why mirror modes are present in planetary magnetosheaths, at comets, and in the heliosheath. Linear theory indicates that the ion cyclotron instability should dominate over the mirror mode instability in electron-proton plasma. In this paper, we take a new approach. We examine the role of plasma electron temperature anisotropy on the ion cyclotron and mirror mode instabilities. It will be shown that an inclusion of anisotropic electrons with T⊥ e/T∥ e ≥ 1.2 reduces the ion cyclotron growth rate substantially and increases the mirror mode growth rate. The minimum plasma beta for mirror instability dominance (over the ion cyclotron instability) is βp = 0.5.en_US
dc.identifier.accession091327
dc.identifier.citationJGR, v.118/2, p.785–793, 2013, doi: 10.1002/jgra.50091en_US
dc.identifier.urihttp://library.iigm.res.in:4000/handle/123456789/659
dc.language.isoenen_US
dc.subjectPlanetary magnetosheathsen_US
dc.subjectIon cyclotronen_US
dc.subjectIon temperatureen_US
dc.subjectElectron-proton plasmaen_US
dc.titleIon temperature anisotropy instabilities in planetary magnetosheathsen_US
dc.typeArticleen_US

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