Ion temperature anisotropy instabilities in planetary magnetosheaths

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dc.contributor.author Remya, B.
dc.contributor.author Reddy, R.V.
dc.contributor.author Tsurutani, B.T.
dc.contributor.author Lakhina, G.S.
dc.contributor.author Echer, E.
dc.date.accessioned 2015-10-27T07:16:33Z
dc.date.accessioned 2021-02-12T09:31:57Z
dc.date.available 2015-10-27T07:16:33Z
dc.date.available 2021-02-12T09:31:57Z
dc.date.issued 2013
dc.identifier.citation JGR, v.118/2, p.785–793, 2013, doi: 10.1002/jgra.50091 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/659
dc.description.abstract There 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.language.iso en en_US
dc.subject Planetary magnetosheaths en_US
dc.subject Ion cyclotron en_US
dc.subject Ion temperature en_US
dc.subject Electron-proton plasma en_US
dc.title Ion temperature anisotropy instabilities in planetary magnetosheaths en_US
dc.type Article en_US
dc.identifier.accession 091327


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