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- W2000685986 abstract "The temperature profiles obtained from holes Dětřichov (north Moravia) and Holubov (south Bohemia) were investigated to extract information on climatic variations. The method of analyzing the data is based on the solution of the heat conduction equation in a horizontally stratified medium subject to a step-function change of the surface temperature, and on the generalized least squares inversion theory. The log from Dětřichov displays a systematic gradient increase to 2 km. Its interpretation is rather ambiguous due to the uncertainty in the thermal conductivity-versus-depth function. Of the conductivity models considered, the homogeneous one yields the most probable results. They suggest the surface warming from −6°C to 7°C 12,000 years ago, which can be related to the climate change at the end of the last glacial period. The curve from Holubov exhibits a gradient increase, which stops at 400 m. It can be explained as a consequence of 0.9 K warming 480 years ago, possibly connected with deforestation of the region during the medieval colonization. Namely, the mean annual soil temperature is by 1K lower in a forest compared with a grass cover in these latitudes. The uppermost 80 m of the record suggest 0.5K cooling 40 years ago, followed by a warming of 1.3K 10 years ago. The two last changes, if true, do not correlate with the climatic variations observed and may reflect some local effects." @default.
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- W2000685986 date "1992-12-01" @default.
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- W2000685986 title "Evidence of ground surface temperature changes from two boreholes in the Bohemian Massif" @default.
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- W2000685986 doi "https://doi.org/10.1016/0031-0182(92)90198-e" @default.
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