A Review of Water Isotopes in Atmospheric General Circulation Models: Recent Advances and Future Prospects
Figure 8
Annual mean D-excess as a function of annual mean δD in precipitation in Antarctica, in the data from Masson-Delmotte et al. [56] (green) and in LMDZ-iso free simulations (blue and red). In blue, the supersaturation is set to its typical value of 0.004, whereas in red it is set to 0.002. This figure is adapted from Risi et al. [24].
