L. Bodri et V. Cermak, CLIMATE CHANGES OF THE LAST 2 MILLENNIA INFERRED FROM BOREHOLE TEMPERATURES - RESULTS FROM THE CZECH-REPUBLIC .2., Global and planetary change, 14(3-4), 1997, pp. 163-173
Borehole temperature logs are indicators of the temperature variations
associated with the past climate change. Temperature-depth records fr
om 98 holes drilled on the territory of the Czech Republic were invert
ed to assess the ground surface temperature history. For most borehole
s the climatic episodes over the two past millennia were identified, i
ncluding warmer period around 400 A.D., followed by colder times betwe
en 700-1000 A.D., the Little Climatic Optimum with its culmination aro
und 1250 +/- 50 A.D., and the Little Ice Age with a temperature minimu
m at 1650 +/- 30 A.D. Since the beginning of the 19th century a genera
l warming has dominated the climate pattern interrupted by several sho
rt-term oscillations, The characteristic times of the minimum (min) an
d maximum (max) alternating extremes are: max 1730 +/- 20, min 1780 +/
- 10, max 1820 +/- 10, min 1880 +/- 10, max 1935 +/- 7, min 1943 +/- 5
, max 1976 +/- 3 A.D. The results are in good agreement with the long-
term meteorological observations and proxy climatic records. As to the
recent general warming trend (last about 30 yr), there exists a certa
in geographical pattern of regions where the rate of warming was parti
cularly intense or where it was relatively weaker possibly indicating
a certain impact of human activities, The highest amount of warming of
2.6-2.8 K were obtained for the industrial regions of the Praha, nort
hern Bohemia and Ostrava coal basins, while the lowest warming of 0.07
-0.6 K corresponds to the southwestern and southern slopes of the Bohe
mian Massif, areas are generally forested.