Diurnal harmonics of Schumann resonance parameters have been studied for th
e first time using data obtained at two sites on opposite hemispheres, Anta
rctica and Greenland. Signatures of a 24-h, a 12-h, and a 8-h harmonic are
clearly discernible in both data sets, but with different strength. The amp
litude of the harmonics changes with season as well. The data can partly be
explained on the basis of current understanding of Schumann resonances. Th
eir properties are determined by the global lightning activity and by the c
ondition of the upper boundary of the Earth-ionosphere wave guide. Since at
mospheric tides are very important for the dynamics ol the D region/mesosph
ere, some of the results may be explained in terms of these waves.