Origin of low proton‐to‐electron temperature ratio in the Earth's plasma sheet

Origin of low proton‐to‐electron temperature ratio in the Earth's plasma sheet

We study the proton‐to‐electron temperature ratio (Tp/Te) in the plasma sheet (PS) of the Earth's magnetotail using 5 years of Cluster observations (2001–2005). The PS intervals are searched within a region defined with −19 

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Veröffentlicht in:Journal of geophysical research. Space physics 2016-10, Vol.121 (10), p.9985-10,004
Hauptverfasser: Grigorenko, E. E., Kronberg, E. A., Daly, P. W., Ganushkina, N. Yu, Lavraud, B., Sauvaud, J.‐A., Zelenyi, L. M.
Format: Artikel
Sprache:eng
Schlagworte:
Broadband
Bursts
Cyclotrons
Earth
Electron energy
Electron heating
Emissions
Frequency ranges
Gyrofrequency
Harmonics
Heating
Intervals
magnetotail
Magnetotails
Plasma
Plasma (physics)
plasma heating
plasma Sheet
Plasmas (physics)
Sciences of the Universe
Sheets
Temperature
Temperature ratio
Turbulence
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Zusammenfassung:We study the proton‐to‐electron temperature ratio (Tp/Te) in the plasma sheet (PS) of the Earth's magnetotail using 5 years of Cluster observations (2001–2005). The PS intervals are searched within a region defined with −19 
ISSN:2169-9380
2169-9402
DOI:10.1002/2016JA022874