@article{oai:nagoya.repo.nii.ac.jp:00019545,
 author = {NAKAI, TAKETOSI},
 journal = {Proceedings of the Research Institute of Atmospherics, Nagoya University},
 month = {Mar},
 note = {The effective height of reflection (h) in the ionosphere and the distance of the source (d) were estimated by the reflection theory in the use of the waveforms of the regular peaked type observed in Toyokawa in 1950 June; h is found to be about 85 ± 5km and d is estimated to the accuracy which is approximately proportional to the reciprocal of the distance of propagation. The derived values for d were compared with good quality C. R. D. F. Fixes and the results showed fair agreement. These results are described in this paper, but particular emphasis is given to a possible range of solutions for h and d deduced by a graphical method of analysis or deduced from the reflection theory and it is discussed that practicability of estimating h or d to a useful accuracy from the waveforms reflected in the ionosphere depends on the distance itself or the number of recorded echoes and the discrepancies which occur between the recorded and ideal sequences of echoes.},
 pages = {20--28},
 title = {THE DISTANCE OF THE SOURCE AND THE HEIGHT OF REFLECTION DEDUCED FROM THE WAVEFORMS OF IONOSPHERIC REFLECTION TYPE},
 volume = {4},
 year = {1957}
}