In this study air and ground temperature measurements taken over a 3-year period in a virgin peat bog are compared with similar measurements taken at nearby mineral soil sites. The purpose of the study was to access the significance of temperature differences that can be expected due to terrain and soil thermal properties. The drainage of cold air into the peat bog was found to be the major factor causing minimum air temperatures to be lower over the bog than at nearby weather stations. The condition of the bog, i.e. whether it was wet or dry, thawing or snow-covered, appeared to have some effect on minimum air temperatures but was not as important a factor as air drainage. Monthly and annual average peat soil temperatures were several degr...
Wetland is known as a source of atmospheric methane, typically produced by microbiological and chem...
Large-scale changes in climate may have many unexpected effects on ecosystems, given the importance ...
Seasonally frozen depth of peat soils in Western Siberia at six oligotrophic forested bogs (ryams) w...
Observations of heat and moisture exchange were made over saturated Sphagnum moss in a grass-covered...
Abstract Detailed, accurate information on soil temperature is crucial for understanding processes ...
Soil temperature strongly influences physical, chemical, and biological activities in soil. However,...
The soil temperature at depths of 20, 50 and 100 cm has been higher in the summertime in the cultiva...
The theory of conductive heat transfer cannot explain different attenuations of the daily amplitude ...
Hydrology controls the physical, chemical and biological processes in peatlands and hence could be t...
We report the results of an investigation on the processes controlling heat transport in peat under ...
ABSTRACT. Strong spatial‘and temporal variations in temperature and effective thermal diffusivity ar...
Reports Canadian Defence Research Board's study, 1950-54. Experiments on rates of freeze and thaw of...
During the summer of 1959 and 1960, field observations of the influence of some climatic and terrain...
Peatlands are considered to be valuable ecosystems on the Planet and play an important role in many ...
The correct determination of evapotranspiration is critical for the calculation of the water balance...
Wetland is known as a source of atmospheric methane, typically produced by microbiological and chem...
Large-scale changes in climate may have many unexpected effects on ecosystems, given the importance ...
Seasonally frozen depth of peat soils in Western Siberia at six oligotrophic forested bogs (ryams) w...
Observations of heat and moisture exchange were made over saturated Sphagnum moss in a grass-covered...
Abstract Detailed, accurate information on soil temperature is crucial for understanding processes ...
Soil temperature strongly influences physical, chemical, and biological activities in soil. However,...
The soil temperature at depths of 20, 50 and 100 cm has been higher in the summertime in the cultiva...
The theory of conductive heat transfer cannot explain different attenuations of the daily amplitude ...
Hydrology controls the physical, chemical and biological processes in peatlands and hence could be t...
We report the results of an investigation on the processes controlling heat transport in peat under ...
ABSTRACT. Strong spatial‘and temporal variations in temperature and effective thermal diffusivity ar...
Reports Canadian Defence Research Board's study, 1950-54. Experiments on rates of freeze and thaw of...
During the summer of 1959 and 1960, field observations of the influence of some climatic and terrain...
Peatlands are considered to be valuable ecosystems on the Planet and play an important role in many ...
The correct determination of evapotranspiration is critical for the calculation of the water balance...
Wetland is known as a source of atmospheric methane, typically produced by microbiological and chem...
Large-scale changes in climate may have many unexpected effects on ecosystems, given the importance ...
Seasonally frozen depth of peat soils in Western Siberia at six oligotrophic forested bogs (ryams) w...