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Whistler Waves Driven by Anisotropic Strahl Velocity Distributions: Cluster Observations
[摘要] Observed properties of the strahl using high resolution 3D electron velocity distribution data obtained from the Cluster/PEACE experiment are used to investigate its linear stability. An automated method to isolate the strahl is used to allow its moments to be computed independent of the solar wind core+halo. Results show that the strahl can have a high temperature anisotropy (T(perpindicular)/T(parallell) approximately > 2). This anisotropy is shown to be an important free energy source for the excitation of high frequency whistler waves. The analysis suggests that the resultant whistler waves are strong enough to regulate the electron velocity distributions in the solar wind through pitch-angle scattering
[发布日期] 2010-01-01 [发布机构] 
[效力级别]  [学科分类] 地质物理学
[关键词]  [时效性] 
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