Instability-Driven Limits on Ion Temperature Anisotropy in the Solar Wind: Observations and Linear Vlasov Theory

Kinetic microinstabilities in the solar wind arise when its non-thermal properties become too extreme. This thesis project focused specifically on the four instabilities associated with ion temperature anisotropy: the cyclotron, mirror, and parallel and oblique firehose instabilities. Numerous stu...

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Main Author: Maruca, Bennett Andrew
Other Authors: Kasper, Justin C.
Language:en_US
Published: Harvard University 2012
Subjects:
Online Access:http://dissertations.umi.com/gsas.harvard:10457
http://nrs.harvard.edu/urn-3:HUL.InstRepos:9547903
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spelling ndltd-harvard.edu-oai-dash.harvard.edu-1-95479032015-08-14T15:41:36ZInstability-Driven Limits on Ion Temperature Anisotropy in the Solar Wind: Observations and Linear Vlasov TheoryMaruca, Bennett Andrewastrophysicsplasma physicsKinetic microinstabilities in the solar wind arise when its non-thermal properties become too extreme. This thesis project focused specifically on the four instabilities associated with ion temperature anisotropy: the cyclotron, mirror, and parallel and oblique firehose instabilities. Numerous studies have provided evidence that proton temperature anisotropy in the solar wind is limited by the actions of these instabilities. For this project, a fully revised analysis of data from the Wind spacecraft's Faraday cups and calculations from linear Vlasov theory were used to extend these findings in two respects. First, theoretical thresholds were derived for the \(\alpha\)-particle temperature anisotropy instabilities, which were then found to be consistent with a statistical analysis of Wind \(\alpha\)-particle data. This suggests that \(\alpha\)-particles, which constitute only about 5% of ions in the solar wind, are nevertheless able to drive temperature anisotropy instabilities. Second, a statistical analysis of Wind proton data found that proton temperature was significantly enhanced in plasma unstable due to proton temperature anisotropy. This implies that extreme proton temperature anisotropies in solar wind at 1 AU arise from ongoing anisotropic heating (versus cooling from, e.g., CGL double adiabatic expansion). Together, these results provide further insight into the complex evolution of the solar wind's non-fluid properties.AstronomyKasper, Justin C.2012-09-12T18:11:32Z2012-09-1220122012-09-12T18:11:32ZThesis or DissertationMaruca, Bennett Andrew. 2012. Instability-Driven Limits on Ion Temperature Anisotropy in the Solar Wind: Observations and Linear Vlasov Theory. Doctoral dissertation, Harvard University.http://dissertations.umi.com/gsas.harvard:10457http://nrs.harvard.edu/urn-3:HUL.InstRepos:9547903en_USopenhttp://nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of-use#LAAHarvard University
collection NDLTD
language en_US
sources NDLTD
topic astrophysics
plasma physics
spellingShingle astrophysics
plasma physics
Maruca, Bennett Andrew
Instability-Driven Limits on Ion Temperature Anisotropy in the Solar Wind: Observations and Linear Vlasov Theory
description Kinetic microinstabilities in the solar wind arise when its non-thermal properties become too extreme. This thesis project focused specifically on the four instabilities associated with ion temperature anisotropy: the cyclotron, mirror, and parallel and oblique firehose instabilities. Numerous studies have provided evidence that proton temperature anisotropy in the solar wind is limited by the actions of these instabilities. For this project, a fully revised analysis of data from the Wind spacecraft's Faraday cups and calculations from linear Vlasov theory were used to extend these findings in two respects. First, theoretical thresholds were derived for the \(\alpha\)-particle temperature anisotropy instabilities, which were then found to be consistent with a statistical analysis of Wind \(\alpha\)-particle data. This suggests that \(\alpha\)-particles, which constitute only about 5% of ions in the solar wind, are nevertheless able to drive temperature anisotropy instabilities. Second, a statistical analysis of Wind proton data found that proton temperature was significantly enhanced in plasma unstable due to proton temperature anisotropy. This implies that extreme proton temperature anisotropies in solar wind at 1 AU arise from ongoing anisotropic heating (versus cooling from, e.g., CGL double adiabatic expansion). Together, these results provide further insight into the complex evolution of the solar wind's non-fluid properties. === Astronomy
author2 Kasper, Justin C.
author_facet Kasper, Justin C.
Maruca, Bennett Andrew
author Maruca, Bennett Andrew
author_sort Maruca, Bennett Andrew
title Instability-Driven Limits on Ion Temperature Anisotropy in the Solar Wind: Observations and Linear Vlasov Theory
title_short Instability-Driven Limits on Ion Temperature Anisotropy in the Solar Wind: Observations and Linear Vlasov Theory
title_full Instability-Driven Limits on Ion Temperature Anisotropy in the Solar Wind: Observations and Linear Vlasov Theory
title_fullStr Instability-Driven Limits on Ion Temperature Anisotropy in the Solar Wind: Observations and Linear Vlasov Theory
title_full_unstemmed Instability-Driven Limits on Ion Temperature Anisotropy in the Solar Wind: Observations and Linear Vlasov Theory
title_sort instability-driven limits on ion temperature anisotropy in the solar wind: observations and linear vlasov theory
publisher Harvard University
publishDate 2012
url http://dissertations.umi.com/gsas.harvard:10457
http://nrs.harvard.edu/urn-3:HUL.InstRepos:9547903
work_keys_str_mv AT marucabennettandrew instabilitydrivenlimitsoniontemperatureanisotropyinthesolarwindobservationsandlinearvlasovtheory
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