Anne Mouchet

TL;DR: 13 models of the ocean–carbon cycle are used to assess calcium carbonate saturation under the IS92a ‘business-as-usual’ scenario for future emissions of anthropogenic carbon dioxide and indicate that conditions detrimental to high-latitude ecosystems could develop within decades, not centuries as suggested previously.

TL;DR: Fenton et al. as mentioned in this paper synthesize estimates of the contemporary net air-sea CO2 flux on the basis of an inversion of interior ocean carbon observations using a suite of 10 ocean general circulation models and compare them to estimates based on a new climatology of the airsea difference of the partial pressure of CO2 (pCO2) (Takahashi et al., 2008).

TL;DR: In this paper, the authors found that the greatest anthropogenic CO2 uptake occurs in the Southern Ocean and in the tropics, and that the global uptake scales approximately linearly with changes in the global CO2 inventory.

TL;DR: In this paper, the authors used radiocarbon and chlorofluorocarbon-11 data from the World Ocean Circulation Experiment (WOCE) to assess a suite of 19 ocean carbon cycle models.

TL;DR: LOVECLIM 1.2 as discussed by the authors is a 3D Earth system model of intermediate complexity, which includes representations of the atmosphere, the ocean and sea ice, the land surface (including vegetation), the ice sheets, the icebergs and the carbon cycle.