SATELLITE OBSERVATIONS OF ELECTRON CONTENT AT THE MAGNETIC EQUATOR
Electron content at the magnetic equator satellite observations
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Electron content at the magnetic equator satellite observations
Ionospheric electron content measurements at magnetic equator obtained by Faraday rotation data analysis from radio beacon satellite
Traveling ionospheric disturbances at magnetic equator, determining electron concentration profiles by incoherent scatter radar
Calculation of ionospheric electron density at the magnetic equator by measuring the polarization rotation of high frequency radio waves from the transit 4a satellite
Omnidirectional electron intensities in the outer belt at earths magnetic equator
Local-time dependence of outer radiation zone electron intensities near magnetic equator
Vertical ionospheric motions near magnetic equator measured by Doppler shifts of incoherent scatter frequency spectra
Daytime D region electron density profiles at magnetic equator from ARCAS flights
Ionospheric electron content variation with solar radio flux from Faraday rotation data at magnetic equator
Outer radiation zone electrons omnidirectional intensity contours at magnetic equator
Nightime electric fields and vertical ionospheric drifts near magnetic equator concurrent measurements
The electric fields at the solar activity minimum on the magnetic equator are evaluated based on data from rocket studies of the vertical profiles of the ionospheric-current magnetic fields and electron concentration. The electric field strength is 1-4 X 100 CGSM units. In addition, the electric field has altitude and time distributions. Its maximum is observed at a height of 110 km, and at 90 and 140 km, it is smaller by a factor of 3-4 than at the 110-km height. The maximum values are registered around noon.
New observations of particle and wave data from the magnetic equator from the DE 1 spacecraft are reported. The results demonstrate that the equatorial plasma population is predominantly hydrogen and that the enhanced ion fluxes observed at the equator occur without an increase in the total plasma density. Helium is occasionally found heated along with the protons, and forms about 10 percent of the equatorially trapped population at such times. The heated H(+) ions can be characterized by a bi-Maxwellian with kT(parallel) = 0.5-1.0 eV and kT = 5-50 eV, with a density of 10-100/cu cm. The total plasma density is relatively constant with latitude. First measurements of the equatorially trapped plasma and coincident UHR measurements show that the trapped plasma is found in conjunction with equatorial noise.
Electron density and electron, ion, and neutral temperature profiles at magnetic equator
Low energy protons omnidirectional intensity contours in outer radiation zone at magnetic equator
Whistler ducts as enhanced ionization from OGO 3 satellite observations near magnetic equator, noting magnetospheric ionization hydrostatic model and predicted cut-off
An intense band of electromagnetic noise is frequently observed near the magnetic equatorial plane at radial distance from about 2 to 5 Re. Recent wideband wave-form measurements with the IMP-6 and Hawkeye-1 satellites have shown that the equatorial noise consists of a complex superposition of many harmonically spaced lines. Several distinctly different frequency spacings are often evident in the same spectrum. The frequency spacing typically ranges from a few Hz to a few tens of Hz. It is suggested that these waves are interacting with energetic protons, alpha particles, and other heavy ions trapped near the magnetic equator. The possible role these waves play in controlling the distribution of the energetic ions is considered.
An intense band of electromagnetic noise is frequently observed near the magnetic equatorial plane at radial distance from about 2 to 9 earth radii. Recent wide band wave form measurements with the Imp 6 and Hawkeye 1 satellites have shown that the equatorial noise consists of a complex superposition of many harmonically spaced lines. Several distinctly different frequency spacings are often evident in the same spectrum. The frequency spacing typically ranges from a few hertz to a few tens of hertz. The purpose of this paper is to suggest that these waves are interacting with energetic protons, alpha particles, and other heavy ions trapped near the magnetic equator. The possible role that these waves play in controlling the distribution of the energetic ions is considered.