The baseline experiment utilized the UFS coupled model Prototype 8, with the exception of employing a coarser 1-degree mesh for the atmospheric, oceanic, and ice models. Additionally, the ocean's initial conditions were from the Ocean Reanalysis System 5. Notably, the tropical SST exhibited an overall positive model bias. Discrepancies in global energy fluxes at both the top and bottom of the model's atmosphere suggest that more attention should be paid to conserving energy, and potentially mass field constituents, in the physics equations.
To investigate deeper into these findings, we conducted a second experiment mirroring the control experiment in all aspects, except for substituting the original NSST (near-surface SST) algorithm, initially designed for uncoupled applications. We implemented a skin temperature scheme that factors in the presence of a multi-layer oceanic mixed layer in MOM6. The outcomes demonstrated a reduction in bias in tropical SST in comparison to the control experiments. This highlights the significance of the positive feedback from ocean skin temperature bias on the coupled system.
- Indicates paper has been withdrawn from meeting
- Indicates an Award Winner