We performed a principal component analysis of observed winter and sum
mer temperature north and south of 55 degrees latitude, in order to ex
amine the spatial and temporal history of long day and night temperatu
res, We used the component weightings calculated from the observed rec
ord to calculate an analogous set of component scores from an infrared
-transient coupled ocean-atmosphere general circulation model (GCM). W
e found no evidence for the increase in the observed night temperature
s that is observed at lower latitudes. Comparison of the observed and
GCM-calculated climate revealed that in only one of forty possible com
ponents were the patterns of observed and calculated climate change si
milar. This behavior is disturbing, because it is at these latitudes t
hat the greatest climatic changes have been predicted to have already
occurred.