Climatic warming in North America: analysis of borehole temperatures
D Deming - Science, 1995 - science.org
Science, 1995•science.org
+ 2-3 r 1912 leading to anomalously high temperatures and an energy imbalance in the
upper 100 m or so of the Earth's crust (7-1 2), Unlike proxy methods for estimating
temperature change (such as tree ring thickness, oxygen isotopes, glacier termini, and so
forth), changes in subsurface temperature are a direct thermophysical consequence of
changes in GST (7). Studies to date have shown that changes in SAT tend to be tracked in
GST changes (10, 13, 14), and
upper 100 m or so of the Earth's crust (7-1 2), Unlike proxy methods for estimating
temperature change (such as tree ring thickness, oxygen isotopes, glacier termini, and so
forth), changes in subsurface temperature are a direct thermophysical consequence of
changes in GST (7). Studies to date have shown that changes in SAT tend to be tracked in
GST changes (10, 13, 14), and
+ 2-3 r 1912 leading to anomalously high temperatures and an energy imbalance in the upper 100 m or so of the Earth's crust (7-1 2), Unlike proxy methods for estimating temperature change (such as tree ring thickness, oxygen isotopes, glacier termini, and so forth), changes in subsurface temperature are a direct thermophysical consequence of changes in GST (7). Studies to date have shown that changes in SAT tend to be tracked in GST changes (10, 13, 14), and
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