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- W2004644660 abstract "Recourse was made to numerical calculations to find the effects of various non-uniform vertical motions due to diffusion, thermal and/or tidal variations on daily variations in the F2-layer. A method of solving the problem was worked out so that the electron density distribution may return back every 24 hr regardless of non-recurrent motions of each part resulted by several causes. The comparison of calculated and observed variations shows that the Bradbury model is better than the Chapman model in every respect. Special emphasis is placed upon the fact that the effect of non-uniform semi-diurnal vertical drift velocities with height gradient of both amplitude and phase is very important except near the equator." @default.
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- W2004644660 date "1959-09-01" @default.
- W2004644660 modified "2023-09-25" @default.
- W2004644660 title "Dynamical structure of the ionospheric F2-layer as deduced from the world-wide daily variations" @default.
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- W2004644660 doi "https://doi.org/10.1016/0021-9169(59)90183-7" @default.
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