The scattered fields for a line source located over a nonuniform stratified earth are computed on the basis of a full wave analysis. It is shown that the radiation pattern is strongly dependent upon the gradient of the overburden depth and that the relative amplitudes of its principal lobes are sensitive to the substratum surface impedance. The frequency of excitation, the angle of incidence, the complex permittivity of the overburden, and the roughness of overburden‐substratum interface are other variable parameters considered in this paper. The relationship between the full wave and geometrical‐optical solutions is also discussed.