E. Guilyardi et al., COUPLED OCEAN-ATMOSPHERE SIMULATION OF CL IMATE VARIABILITY, Comptes rendus de l'Academie des sciences. Serie II. Mecanique, physique, chimie, astronomie, 320(8), 1995, pp. 683-690
A 50-year climatic numerical simulation with a global coupled ocean-at
mosphere general circulation model (CGCM) is presented. The only forci
ng is the input of solar radiation at the top of the atmosphere. After
an initial tropical warming, air-sea fluxes reach a global balance at
the interface. Average oceanic temperature and salinity drifts are re
latively weak (+0.4 degrees C/century and +0.04 g/kg/century). Despite
some systematic biases, the model robustness and stability are quite
promising for future studies.