This work compares the classic Chen and Millero [1979] approach for estimat
ing anthropogenic CO2 from ocean carbon measurements with the more recent D
eltaC* technique used by Sabine et al. [1999] to estimate anthropogenic CO2
concentrations in the Indian Ocean. Application of the Chen technique to t
he WOCE/JGOFS Indian Ocean data set gives a total anthropogenic CO2 invento
ry that is essentially the same as the DeltaC* inventory, but there are sub
stantial differences in the distributions within the water column. Some of
these differences result from details of the application of the techniques
such as the choice of which equation to use for the preformed alkalinity co
ncentration or the choice of stoichiometric ratio to use for the biological
correction. More significant differences, however, result from two fundame
ntal differences in the techniques. One fundamental difference between the
two techniques is that changes in the properties of the subsurface waters a
re referenced to a single deep water value in the Chen approach instead of
the multiple reference points from the isopycnal analysis used in the Delta
C* approach. The second fundamental difference is in the estimation of the
preindustrial TCO2 distribution. Many of the differences examined have coun
teracting effects that may result in a total anthropogenic CO2 inventory th
at is similar for the two techniques. However, this similarity does not imp
ly that both approaches are right. Comparison with global carbon models and
other measurement-based techniques do not clearly demonstrate that one tec
hnique is better than another. However, given the additional constraints of
the transient tracers and the isopycnal analysis, we believe that the Delt
aC* technique provides a more robust estimate.