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This communication compares a more general numerical point-to-point transient wave propagation program to a known analytical (full-wave) solution based upon a certain special geometry and ionospheric profile. The main purpose of the comparison is that of using the known analytical results as a test case for the numerical program. The parameters of the ionosphere were chosen to purposively tax the condition of requiring a slowly varying medium in using the Wentzel-Kramer-Brillouin (WKB) method (i.e., the parameters chosen lead to a sporadicE-type layer). With the results favorable for this case, the application of a numerical procedure, based upon the WEB method, to the more slowly varyingFregion would definitely be acceptable. Based upon the full-wave and WKB solutions, results are given in the form of time-domain waveforms due to reflection of a transient wave from the ionosphere.
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J. Linsay (1971) studied this question.
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