Solar wind proton temperature anisotropy: Linear theory and WIND/SWE observations
摘要:
We present a comparison between WIND/SWE observations [Kasper et al., 2006] of β p and T ⊥p /T p (where β p is the proton parallel beta and T ⊥p and T p are the perpendicular and parallel proton temperatures, respectively; here parallel and perpendicular indicate directions with respect to the ambient magnetic field) and predictions of the Vlasov linear theory. In the slow solar wind, the observed proton temperature anisotropy seems to be constrained by oblique instabilities, by the mirror one and the oblique fire hose, contrary to the results of the linear theory which predicts a domi-nance of the proton cyclotron instability and the parallel fire hose. The fast solar wind core protons exhibit an anticorrelation between β c and T ⊥c /T c (where β c is the core proton parallel beta and T ⊥c and T c are the perpendicular and parallel core proton temper-atures, respectively) similar to that observed in the HELIOS data [Marsch et al., 2004].
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关键词:
peraluminous granite geochronology geochemistry petrogenesis arc-continent collision continental growth extensional collapse
DOI:
10.1029/2006GL025925
被引量:
年份:
2006
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