1967 Volume 45 Issue 4 Pages 332-341
The distribution of the atmospheric refractive index was observed repeatedly at eleva-tions up to 3Km over the course between Tokyo and Sendai. UHF propagation experiment was also conducted over the 310Km land-path between Tokyo and Sendai. Considering the effect of mountain wave which was caused by the gently sloped mountain ridge near the midpoint of the course, meteorological interpretation was made on both the observed N-profiles and the spatial distribution of ΔN2. The influence of the airflow across a mountain ridge on the variation of the UHF transmission loss, L, was also investigated by the use of the upper meteorological data. Correlation between the observed hourly median values of L and the relative values of the scattering cross section, a, estimated by the upper meteorological data is fairly good.