The ground surface temperature (GST) history in NW Italy was reconstructed
for the last three centuries by means of temperature-depth data recorded in
a borehole in 1982. The results indicate relatively warmer periods in the
18th century and at the end the 1970s. A more recent set of underground tem
perature data was recorded in 1996. The comparison with the earlier thermal
logging shows an evident temperature increase in the uppermost 80 m. Two d
ifferent inversion techniques yield a subsurface temperature increase of 0.
8-1.0 K since the 1980s. The inferred climatic model is consistent with the
air temperature variations recorded at the Genoa University meteorological
station. (C) 2000 Elsevier Science B.V. All rights reserved.