The heat exchange at the air/ground interface is determined by many complex
processes making the energy balance at the earth's surface extremely diffi
cult to quantify and model. A new methodology allows heat flux at the Earth
's surface to be estimated using ground surface temperature history reconst
ructed from geothermal data. We found that over a large region in eastern a
nd central Canada, the average heat flux into the ground during the last 10
00 years was on the order of 2.8 mWm(-2). Our results suggest that signific
ant change in the ground heat flux occurred in the last two centuries. The
200 years averaged heat flux since 1765 is 17.0 mWm(-2), while the average
heat flux over the latest 100 years is 74.0 mWm(-2). The sensitivity of the
subsurface to very small energy imbalances makes these type of data and an
alysis useful complements to the paleoclimatic record; they also provide co
nstrains for general circulation model land-surface parameterization over a
wide range of spatial-temporal scales.