Results 181 to 190 of about 114,060 (217)
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The equatorial F-region of the ionosphere
Journal of Atmospheric and Terrestrial Physics, 1960Abstract A comparison of data from ionospheric sounders at Chimbote and Panama, shows that afternoon critical frequencies in the equatorial zone are negatively correlated with those on the same meridian in the sub-tropical belts. This supports Martyn's suggestion that ionization is transported from the equatorial zone to the sub-tropics.
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Dispersive motions in the equatorial ionosphere
Radio Science, 1974The results of the dispersion analysis of the spaced receiver records of fading for an equatorial station in the Indian zone are discussed. It is shown that the apparent drift speed increases almost linearly with the frequency of fading in all the cases studied for both the E and F regions.
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The elongation of irregularities in the equatorial ionosphere
Journal of Geophysical Research, 1963A correlation analysis of spaced aerial fading measurements for medium-frequency radio waves scattered from the D and E regions at a location near the magnetic equator is reported. The results show that there is a slight tendency towards field-aligned elongation of the diffraction pattern on the ground for echoes from 80 and 90 km and considerable ...
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Space Weather in the Equatorial Ionosphere
Space Science Reviews, 2003The’ scintillations’ observed on signals received in the equatorial region from GPS satellites are due to plasma instabilities in the F region of the ionosphere, also detected as spread F These instabilities give rise to depletions of ionisation or ‘bubbles’.
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The integrated electron content in the equatorial ionosphere
Journal of Atmospheric and Terrestrial Physics, 1967Abstract It is shown that an equatorial anomaly exists in the electron content of the topside ionosphere such that the electron content during the early afternoon is greater at latitudes north and south of the magnetic equator than at the equator itself.
J.W. King +3 more
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Equatorial hiss in the topside ionosphere
Journal of Geophysical Research: Space Physics, 1979Equatorial hiss seen in the topside ionosphere by the Dartmouth experiment on Ogo 6, using an electric dipole antenna, is described. The observations are consistent with wave normal positions intermediate between the geomagnetic field and the resonance cone.
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Atmospheric waves and the equatorial ionosphere
Journal of Atmospheric and Terrestrial Physics, 1977Abstract Rotational effects due to the meridional gradient of the Coriolis parameter produce a class of equatorial gravity waves whose dispersion properties resemble those of acoustic waves. Supersonic sources near the equator should then be able to excite these equatorial waves.
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Topside irregularities in the equatorial ionosphere
Journal of Atmospheric and Terrestrial Physics, 1977Abstract This paper is a brief review of ionospheric irregularities in the equatorial topside ionosphere. Results from topside sounders, direct measurement satellites, and the Jicamarca incoherent scatter radar are discussed. Scintillation observations and theories of irregularities are not discussed in detail as these are the subject of other review
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Equion, an Equatorial Ionospheric Irregularity Experiment
Journal of Geophysical Research, 1977Abstract : This paper describes a coordinated rocket and ground based study to investigate Equatorial Spread-F irregularities. Measurements by the Jicamarca backscatter radar, ionosondes, airglow instrumentation and of radio scintillations were correlated with high spatial resolution measurements of electron densities, particle fluxes and VLF-ELF ...
F. A. Morse +11 more
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Equatorial electrojet—II. Use of the model to study the equatorial ionosphere
Journal of Atmospheric and Terrestrial Physics, 1973Abstract Observations of the electrojet are examined in conjunction with a numerical physical model developed in a companion paper. The model reproduces the basic features of the observed electrojet, but certain discrepancies suggest that the assumptions of the model or the conductivity distributions used may be inaccurate.
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