Lack of a 19th-century baseline temperature against which 20th-century
warming can be referenced constitutes a deficiency in understanding r
ecent climate change. Combination of borehole temperature profiles, wh
ich contain a memory of surface temperature changes in previous centur
ies, with the meteorological archive of surface air temperatures can p
rovide a 19th-century baseline temperature tied to the current observa
tional record. A test case in Utah, where boreholes are interspersed w
ith meteorological stations belonging to the Historical Climatological
Network, yields a noise reduction in estimates of 20th-century warmin
g and a baseline temperature that is 0.6 degrees +/- 0.1 degrees C bel
ow the 1951 to 1970 mean temperature for the region.