We construct an extratropical reduced temperature–depth profile for land areas north
of 20°N latitude from the global borehole temperature database compiled for climate
reconstruction. The mean reduced temperature profile compares well with a time series
constructed from an initial baseline temperature (0.6° ± 0.1°C) and the last 140 years
of...
Temperature profiles from boreholes on the Colorado Plateau of southeastern Utah have been examined for evidence of climate change. Because these boreholes penetrate layered sedimentary rocks with different thermal conductivities, Bullard plots (temperature versus integrated thermal resistance) are used to estimate background heat flow and surface temperature intercepts. Reduced temperatures,...
Long-period ground surface temperature variations contained in borehole
temperature-depth profiles form a complementary climate change record to high-frequency,
but noisy surface air temperature (SAT) records at weather stations. We illustrate the
benefits of jointly analyzing geothermal and meteorological data for two regions in Utah
where both high-quality temperature-depth measurements and...
Temperature profiles from boreholes on the Colorado Plateau of southeastern Utah
have been examined for evidence of climate change. Because these boreholes penetrate layered
sedimentary rocks with different thermal conductivities, Bullard plots (Temperature versus
integrated thermal resistance) are used to estimate background heat flow and surface temperature
intercepts. Reduced temperatures,...
The southern portion of the Kodiak-Bowie seamonnt chain in the southeastern
Gulf of Alaska presents a unique opportunity to investigate loading on young oceanic
lithosphere. Oceanic lithosphere younger than 25 Ma is loaded both by sediments in a deep
offshore trough and by seamount 100-200 km offshore. Free-air gravity anomaly...
Temperature-depth profiles in borehole CC-I, northwestern Utah, were measured in 1978, 1990, and 1992. Borehole temperatures below 80 m depth are highly reproducible over the 14 year period indicating long term thermal stability. A slowly changing temperature field above 80 m depth has similiar characteristics to synthetic temperature profiles computed...
Observations of air and ground temperatures collected between 1993 and 2004 from Emigrant Pass Geothermal Climate Observatory in northwestern Utah are analyzed to understand the relationship between these two quantities. The influence of surface air temperature (SAT), incident solar radiation, and snow cover on surface ground temperature (SGT) variations are...
Borehole temperature profiles provide a record of ground surface temperature (GST)
change at the decadal to centennial time scale. GST histories reconstructed from boreholes
are particularly useful in climate reconstruction if changes in GST and surface air
temperature (SAT) are effectively coupled at decadal and longer time periods and it...
Changes in snow’s influence on surface ground temperature (SGT) could create a bias
in the borehole temperature record of climate change. Using a snow-ground thermal model
which predicts changes in the mean annual offset between SGT and surface air
temperature (SAT), we calculate the response of SGT to changes in...
[1] Borehole temperature-depth profiles contain a record of surface ground temperature
(SGT) changes with time and complement surface air temperature (SAT) analysis to infer
climate change over multiple centuries. Ground temperatures are generally warmer than
air temperatures due to solar radiation effects in the summer and the insulating effect
of...