Results 181 to 190 of about 2,664 (215)
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Traveling disturbances originating in the outer ionosphere
Journal of Geophysical Research, 1959Some observations that have been obtained with variations of the classical echo-sounding method must be interpreted as resulting from perturbation and/or oscillation phenomena occurring in the outer ionosphere. The vertical velocity component of ‘traveling disturbances’ coming from outside and propagating through the ionosphere is determined as 115±35 ...
K. Bibl, K. Rawer
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Traveling ionospheric disturbances associated with nuclear detonations
Journal of Geophysical Research, 1967The analysis of ionospheric data taken from 54 ionosonde observatories throughout the world indicates the presence of several traveling ionospheric disturbances originating from the five high-altitude nuclear tests conducted over Johnston Island in 1962.
W. J. Breitling +2 more
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Incoherent scatter observations of traveling ionospheric disturbances
Journal of Geophysical Research, 1964The incoherent scatter technique is used to study large-scale traveling ionospheric disturbances above Puerto Rico. Below the F-region maximum the measurements of disturbance amplitude, period, and direction of phase progression with time (downward) are consistent with the bottomside results of other workers. Above the maximum, however, the surfaces of
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Evidence of Directional Filtering of Travelling Ionospheric Disturbances
Nature Physical Science, 1972IT has recently been pointed out1 that the strong thermospheric winds would act as a directional filter. In a windy thermosphere an otherwise penetrating gravity wave may become reflected or asymptotically trapped near the lower thermosphere. Because both reflexion and trapping take place below the ionospheric F2 peak, such waves may not excite ...
K. C. YEH, H. D. WEBB, D. H. COWLING
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Analysis of large-scale traveling ionospheric disturbances
Journal of Geophysical Research, 1964It is shown that an acoustic-gravity wave interpretation of Chan and Villard's observations of large-scale traveling ionospheric disturbances is consistent with theory. By using the dispersion curves and kinetic energy profiles for atmospheric gravity waves recently computed by Pfeffer and Zarichny, Pfeffer and Gersten, and earlier by Press and ...
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Mid-latitude range spread and travelling ionospheric disturbances
Journal of Atmospheric and Terrestrial Physics, 1988This paper first discusses some early results (most hitherto unpublished) on off-vertical reflections which result from tilted isoionic contours associated with the passage of travelling ionospheric disturbances (TIDs). Azimuth of arrival and zenith angle information on these returning signals is discussed together with the role of these signals in ...
Bowman G.G., Monro P.E.
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HF Doppler studies of traveling ionospheric disturbances
Journal of Atmospheric and Terrestrial Physics, 1968Abstract Wavelike ionospheric motions observed with a network of CW Doppler sounders are analyzed and found to fall into four separate classes not previously distinguished. The motions of each type are attributed to various kinds of atmospheric waves that interact with the ionosphere.
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Traveling ionospheric disturbances observed at the magnetic equator
Journal of Geophysical Research, 1971Traveling ionospheric disturbances at magnetic equator, determining electron concentration profiles by incoherent scatter ...
D. L. Sterling, W. H. Hooke, R. Cohen
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Traveling ionospheric disturbances?A review
Radiophysics and Quantum Electronics, 1968B. N. Gershman, G. I. Grigor'ev
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2017
The ionosphere is an electrically charged atmospheric region which is coupled to the sun, the magnetosphere, and the neutral atmosphere. The ionospheric state can significantly impact technological systems, especially those which utilize radio frequency energy.
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The ionosphere is an electrically charged atmospheric region which is coupled to the sun, the magnetosphere, and the neutral atmosphere. The ionospheric state can significantly impact technological systems, especially those which utilize radio frequency energy.
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