Natural ocean carbon cycle sensitivity to parameterizations of the recycling in a climate model

Such differences between low-frequency variations of ocean carbon fluxes and other dynamical fields are even stronger in the Southern Ocean, where Boer (2004) shows that

Another motivation for this work is to have a model that includes a terrestrial scheme, so that the global carbon cycle encompassing the atmosphere, ocean, and land can

FAMOUS (Smith et al., 2008), a coupled atmosphere-ocean general circulation model (GCM) to simulate the global climate of 5 time periods during the last glacial period driven

In this study we use the Pelagic Integration Scheme for Carbon and Ecosystem studies (PISCES) global ocean- biogeochemistry model (Aumont and Bopp, 2006) to exam- ine the response

Latitudinal shifts in the Southern Ocean westerly wind jet could drive changes in the glacial to interglacial ocean CO 2 inventory.. However, whilst CMIP5 model results

To summarize, any global model study that aims to in- versely determine parameters of a global biogeochemical ocean model in an attempt to find the model setup “best” suited for

The ECHAM/MESSy Atmospheric Chemistry (EMAC) model is coupled to the ocean general circulation model MPIOM using the Modular Earth Submodel System (MESSy) interface.. MPIOM is

While enhanced diapycnal mixing between the mixed layer and the isopycnic layer immediately below leads to an increase in export production in the Southern Ocean, it produces the