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Journal ArticleDOI

The ionospheric response to internal gravity waves: 1. The F2 region response

William H. Hooke
- 01 Oct 1970 - 
- Vol. 75, Iss: 28, pp 5535-5544
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TLDR
In this paper, the F2 region ionospheric response to individual internal gravity waves is calculated as a function of the azimuth of wave propagation, and the response is shown to be highly anisotropic, with the anisotropy itself depending on the wave parameters, the geomagnetic dip and the prevailing ionization density gradient.
Abstract
The F2 region ionospheric response to individual internal gravity waves is calculated as a function of the azimuth of wave propagation. This response is shown to be highly anisotropic, with the anisotropy itself depending on the wave parameters, the geomagnetic dip, and the prevailing ionization density gradient. Because the ionization density gradient changes with time of day and season, the ionospheric response and hence the traveling ionospheric disturbance statistics themselves should exhibit corresponding diurnal and seasonal variations. The physical basis for the anisotropy of the ionospheric response is discussed.

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Citations
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Atmospheric gravity waves generated in the high‐latitude ionosphere: A review

TL;DR: A review of theoretical and observational results describing atmospheric gravity wave (AGW)/traveling ionospheric disturbance (TID) phenomena at high latitudes is presented in this paper.
Journal ArticleDOI

Global propagation of atmospheric gravity waves: A review

TL;DR: The theoretical and observational evidence concerning the global propagation of atmospheric gravity waves is reviewed in this article, with special emphasis on the waves generated in the auroral zones, and it is concluded that the only natural sources of large-scale TIDs are in the ionospheric zones.
Journal ArticleDOI

Acoustic‐gravity waves in the upper atmosphere

Kung C. Yeh, +1 more
TL;DR: In this article, the authors review the theory of acoustic-gravity waves, the interaction of such waves with the ionosphere, the experimental support for the existence of acoustic gravity waves in the upper atmosphere, and the role played by acoustic gravity wave in thermospheric dynamics.
Journal ArticleDOI

Directivity and apparent velocity of the coseismic ionospheric disturbances observed with a dense GPS array

TL;DR: In this article, a dense Global Positioning System array was used to detect coseismic uplifts of the sea surface initially as upward propagating compressive pulses of atmosphere, which were gradually refracted to propagate horizontally in ionosphere.
Journal ArticleDOI

Internal wave coupling processes in Earth's atmosphere

TL;DR: A review of vertical coupling in the atmosphere and ionosphere system induced by internal waves of lower atmospheric origin is presented in this article, focusing on gravity waves, solar tides, planetary Rossby and Kelvin waves.
References
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Journal ArticleDOI

Internal atmospheric gravity waves at ionospheric heights

TL;DR: In this paper, the proper interpretation of irregular motions in the upper atmosphere has been investigated by a variety of techniques, but their proper interpretation has yet to be established. But their proper meaning has not yet been established.
Journal ArticleDOI

Ionospheric irregularities produced by internal atmospheric gravity waves

TL;DR: In this article, a perturbation treatment is used to determine the nature and magnitude of the effects of internal atmospheric gravity waves on the ambient rates of production, chemical loss, and motion of the ionization.
Journal ArticleDOI

The upper atmosphere in motion

TL;DR: In this article, a review of the observational evidence for the upper atmosphere is presented, in groupings determined by the physical processes that are thought to be operative, and corresponding theories are measured against it.
Journal ArticleDOI

The viscous damping of atmospheric gravity waves

TL;DR: In this article, the effects of viscous damping and thermal conduction at meteor heights in the upper atmosphere were investigated, and the results of this paper are consistent with the conclusions of an earlier analysis, insofar as the two overlap.
Journal ArticleDOI

On the propagation of atmospheric gravity waves through regions of wind shear

TL;DR: Removal of incident wave spectrum by background wind shears during atmospheric gravity waves propagation to ionosphere from lower regions is discussed in this paper, where the authors consider the case of a single wave.