Record Details

Geothermics and climate change : 1. Analysis of borehole temperatures with emphasis on resolving power

ScholarsArchive at Oregon State University

Field Value
Title Geothermics and climate change : 1. Analysis of borehole temperatures with emphasis on resolving power
Names Harris, Robert N. (creator)
Chapman, David S. (creator)
Date Issued 1998-04-10 (iso8601)
Note copyrighted by American Geophysical Union
Abstract Temperature-depth data from six boreholes in western Utah and nine boreholes in
southeastern Utah are reanalyzed for evidence of ground surface temperature (GST)
histories. We invert the temperature-depth data using the functional space inverse
algorithm of Shen and Beck [1991, 1992J which we prefer over previous inversions of these
data because of its greater sophistication and flexibility in suppressing noise. GST histories
for western and southeastern Utah are generally consistent and suggest that temperatures in
the mid-1800s are, on average, cooler than previous centuries, followed by about 0.6°C of
warming in this century. Attention is given to the temporal resolution of our GST solutions
showing the time-smearing effects of heat conduction on the Solutions. GST solutions
represent an average ground temperature over a time window that expands as we look
farther into the past. The size of the time window is a function of measurement and
geologic noise and limits the ultimate resolution of GST reconstructions.
Genre Article
Identifier Chapman, D. S., Harris, R. N., (1998) Geothermics and climate change 1. analysis of borehole temperatures with emphasis on resolving power, J. Geophys. Res., 103, B4, 7363-7370.

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