Extensive measurements of CO2 fugacity in the North Pacific surface oc
ean and overlying atmosphere during the years 1985-1989 are synthesize
d and interpreted to yield a basin-wide estimate of Delta fCO(2). The
observations, taken from February through early September, suggest tha
t the subtropical and subarctic North Pacific is a small sink for atmo
spheric CO2 (0.07 to 0.2 Gton C (half year)(-1) for the region north o
f 15 degrees N). Objective analysis techniques are used to estimate un
certainty fields resulting from constructing basin-wide contours of oc
eanic fCO(2) on the basis of individual cruise transects. The uncertai
nties are significant and imply that future sampling programs need to
recognize that estimating oceanic uptake of anthropogenic CO2 from shi
p-transect observations of oceanic fCO(2) alone will require very exte
nsive sampling.