A summary of C-14 data from atmospheric sampling and measurements on wood f
rom annual tree rings for the period 1945-1997 AD is presented and evaluate
d. Atmospheric records are characterized by different distributions of bomb
-test C-14 between the Northern and Southern Hemispheres, latitude dependen
ce, and seasonal fluctuations. Radiocarbon data from tree rings are summari
sed and plotted against atmospheric records from similar latitudes. In some
cases, discrepancies are found. Possible reasons for this include: 1) the
use of stored carbohydrate from the previous year, 2) different C-14 levels
in the air around subcanopy trees due to respiration of CO2, 3) regional a
nd local effects of anthropogenic CO2 and C-14 sources, 4) Sampling of wood
material too close to ring boundaries, and 5) insufficient pretreatment of
tree ring samples for dating. But in cases where trees were carefully sele
cted and the samples adequately pretreated, radiocarbon data from tree ring
s show excellent agreement with direct atmospheric sampling records.