Several statistical characteristics of the soil temperature in Athens/
Greece are determined through Fourier analysis of a 74 year record (19
17-1990) of soil temperatures at the surface and at various depths and
for both bare and short-grass-covered areas. Specifically the soil te
mperature patterns are presented along with the Fourier amplitudes and
phases of the most important harmonics. It was found that the first t
hree harmonics can reproduce most of the observed patterns in soil tem
peratures at the surface and at various depths. Finally, the results o
f the present analysis are compared with some existing data from other
known sets of measurements. Copyright (C) 1996 Elsevier Science Ltd.