Abstract
The Community Climate Model at the National Center for Atmospheric Research has been coupled to a simple mixed-layer ocean model and to a coarse-grid ocean general circulation model (OGCM). This paper compares the responses of simulated climate to increases of atmospheric carbon dioxide (CO2) in these two coupled models. These two sets of experiments demonstrate that different ocean models and types of CO2 forcing in the climate system result in different CO2 climate responses. Earlier studies with energy-balance climate models confirm that instantaneous CO2 doubling simulations respond differently than transient simulations. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 79-110 |
| Number of pages | 32 |
| Journal | Unknown Journal |
| State | Published - 1991 |