MMS Observations of Beta-Dependent Constraints on Ion Temperature-Anisotropy in Earth's Magnetosheath
arXiv:1806.08886 · doi:10.3847/1538-4357/aaddfb
Abstract
Protons (ionized hydrogen) in the solar wind frequently exhibit distinct temperatures ( and ) perpendicular and parallel to the plasma's background magnetic-field. Numerous prior studies of the interplanetary solar-wind have shown that, as plasma beta () increases, a narrower range of temperature-anisotropy () values is observed. Conventionally, this effect has been ascribed to the actions of kinetic microinstabilities. This study is the first to use data from the Magnetospheric Multiscale Mission (MMS) to explore such -dependent limits on in Earth's magnetosheath. The distribution of these data across the -plane reveals limits on both and . Linear Vlasov theory is used to compute contours of constant growth-rate for the ion-cyclotron, mirror, parallel-firehose, and oblique-firehose instabilities. These instability thresholds closely align with the contours of the data distribution, which suggests a strong association of instabilities with extremes of ion temperature anisotropy in the magnetosheath. The potential for instabilities to regulate temperature anisotropy is discussed.
arXiv commentSubmitted to The Astrophysical Journal Letters
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Cited by in corpus (8)
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- Observational evidence for solar wind proton heating by ion-scale turbulence
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