Development of a system emulating the global carbon cycle in Earth system models

Sediment CArbon cycle Reservoir (LOSCAR) model (Zeebe et al., 2009; Zeebe, 2012b), we calculate perturbations to at- mosphere temperature, total carbon, ocean temperature, total

For the historical and future simulations (including the emissions driven and de- coupled carbon cycle experiments, and AMIP runs) a time- varying data set of stratospheric ozone

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

The interactive ocean carbon cycle model is the NASA Ocean Biogeochemistry Model (NOBM, (Gregg and Casey, 2007; Romanou et al., 2013), which is interactively coupled to the ocean

Ideally, one would run a very large set of transient simulations of a GCM with interactive carbon-cycle fully coupled to a dy- namic ocean model, simultaneously perturbing all

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

Here we test the linear additivity assumption for changes in global mean temperature and changes in variables of the energy budget and hydrological cycle in a GCM.. The objective

Prominent examples of processes during which isotopic fractionation occurs in our context of global carbon cycle re- search are gas exchange between surface ocean and atmo- sphere