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- W2043933417 abstract "An analysis is performed on ionosonde data produced during five years of operation of an oblique sounder transmitting on a path from Darwin (12.4°S, 130.9°E) to Alice Springs (23.5°S, 133.7°E). It is found that the occurrence of sporadic-E (Es) shows a relatively mild diurnal dependence, with a significant amount of Es occurring in the early evening before midnight. It appears that, on average, nighttime Es produces weaker reflections than daytime Es. The power of the Es reflections as a function of frequency is collated for all ionograms. The resulting power curve exhibits total and partial reflection sections. In trying to reproduce the partial reflection section of the curve it is shown that a layer without horizontal structure is required to be only 100 m thick. A second model involving a layer consisting of horizontally localised clouds of scatterers, with scale sizes ranging from 100 to 1000 metres, reproduces the partial reflection section of the curve quite well. The size, intensity and distribution of the clouds affects the curve shape on individual ionograms, resulting in the suggestion that nighttime layers are more irregular than daytime layers." @default.
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- W2043933417 date "1995-12-01" @default.
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- W2043933417 title "Analysis of Es traces from a calibrated oblique ionosonde" @default.
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- W2043933417 doi "https://doi.org/10.1016/0021-9169(95)00095-j" @default.
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