Electron H/+/ and O/+/ temperatures and densities from Arecibo incoherent-scatter results

Physics

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Hydrogen Ions, Incoherent Scattering, Magnetospheric Electron Density, Magnetospheric Ion Density, Oxygen Ions, Particle Energy, Electron Energy, Ion Temperature, Particle Density (Concentration), Vertical Distribution

Scientific paper

Results are presented from observations of the altitude region 230 to 1200 km above Arecibo on a winter morning. Analysis of autocorrelation functions of theoretical incoherent scatter spectra indicate that the temperatures and densities of the electrons, H(+) and O(+) can be calculated from experimental data. Typical data show that T(H+)/T(O+) has a maximum near 550 km and T(O+) and Te profiles have a temperature gradient at high altitudes of approximately 1 K/km.

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