Figure 13 (Right) Global ocean circulation model results from 12 different coarse-resolution models participating in OCMIP-2
compared to WOCE data for natural D
14 C on a meridional Pacific section. The model groups are identified in each subpanel and in
Table 1 All of the models used the same chemistry and boundary conditions.
RADIOCARBON 247
compared to WOCE data for natural D
14 C on a meridional Pacific section. The model groups are identified in each subpanel and in
Table 1 All of the models used the same chemistry and boundary conditions.
RADIOCARBON 247