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Majority of Solar Wind Intervals Support Ion-Driven Instabilities.
K G Klein1,2, B L Alterman1, M L Stevens3
1Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, Michigan 48109, USA.
Physical Review Letters
|June 5, 2018
Summary
Solar wind stability at 1 AU is statistically assessed using Nyquist
Area of Science:
- Space Physics
- Plasma Physics
- Astrophysics
Background:
- The solar wind is a stream of charged particles released from the upper atmosphere of the Sun, constantly flowing through the solar system.
- Understanding the stability of the solar wind is crucial for comprehending space weather phenomena and plasma behavior in astrophysical environments.
- Previous studies often focused on single free-energy sources, potentially oversimplifying the complex dynamics of solar wind plasma.
Purpose of the Study:
- To statistically assess the stability of the solar wind at 1 Astronomical Unit (AU) against multiple ion free-energy sources.
- To investigate the influence of proton and Helium (He^{2+}) temperature anisotropy and relative drifts on solar wind stability.
- To compare results with traditional threshold models by employing Nyquist's instability criterion.
Main Methods:
- Utilized Nyquist's instability criterion to analyze solar wind plasma stability.
- Modeled solar wind ion components (proton core, proton beam, He^{2+}) as drifting bi-Maxwellians.
- Analyzed 309 randomly selected spectra from the Wind spacecraft data.
Main Results:
- 53.7% of analyzed spectra were found to be unstable when considering multiple free-energy sources.
- Only 4.5% of spectra exhibited instability towards long-wavelength perturbations.
- Instabilities were predominantly associated with resolved proton beams, large He^{2+} drift speeds, and proton temperature anisotropy.
Conclusions:
- The solar wind exhibits significant instability when multiple free-energy sources, including temperature anisotropies and ion drifts, are considered.
- Long-wavelength instabilities are rare, suggesting a relative stability against large-scale perturbations.
- Observed instabilities generally possess slow growth rates, indicating they may not significantly impact short-term kinetic-scale processes.
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