Characteristics of a reflecting layer below the classical D region

Details Characteristics of a reflecting layer below the classical D region Characteristics of a reflecting layer below the classical D region

Nov 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987jgr....9212443b&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 92, Nov. 1, 1987, p. 12443, 12444.

Computer Science

Sound

D Region, Ground Wave Propagation, Ionospheric Sounding, Very Low Frequencies, Wave Reflection, Daytime, Geomagnetism

Scientific paper

Rasmussen et al. (1980) described low-altitude reflections observed with a VLF/LF ionospheric sounder, apparently from a C layer, which could be interpreted as having come from ionospheric layers of constant conductivity. In the example given in their paper, they found a layer that extended from 63 to 69 km in height. This brief paper presents an improved method for calculating such layers which shows that, in fact, the best fitting layer for their example extends from 60 to 66 km.

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