Deep water formation in the North Atlantic Ocean in high resolution global coupled climate models

• Main Authors: Koenigk, Torben, Fuentes-Franco, Ramon, Meccia, Virna, Gutjahr, Oliver, Jackson, Laura C., New, Adrian L., Ortega, Pablo, Roberts, Christopher, Roberts, Malcolm, Arsouze, Thomas, Iovino, Doroteaciro, Moine, Marie-Pierre, Sein, Dmitry V.
• Format: Text
• Language: English
• Published: 2020
• Subjects: Greenland; Greenland Sea; Labrador Sea; North Atlantic
• Online Access: https://doi.org/10.5194/os-2020-41; https://os.copernicus.org/preprints/os-2020-41/

Simulations from seven global coupled climate models performed at high and standard resolution as part of the High Resolution Model Intercomparison Project (HighResMIP) have been analyzed to study the impact of horizontal resolution in both ocean and atmosphere on deep ocean convection in the North Atlantic and to evaluate the robustness of the signal across models. The representation of convection varies strongly among models. Compared to observations from ARGO-floats, most models substantially overestimate deep water formation in the Labrador Sea. In the Greenland Sea, some models overestimate convection while others show too weak convection. In most models, higher ocean resolution leads to increased deep convection in the Labrador Sea and reduced convection in the Greenland Sea. Increasing the atmospheric resolution has only little effect on the deep convection, except in two models, which share the same atmospheric component and show reduced convection. Simulated convection in the Labrador Sea is largely governed by the release of heat from the ocean to the atmosphere. Higher resolution models show stronger surface heat fluxes than the standard resolution models in the convection areas, which promotes the stronger convection in the Labrador Sea. In the Greenland Sea, the connection between high resolution and ocean heat release to the atmosphere is less robust and there is more variation across models in the relation between surface heat fluxes and convection. Simulated freshwater fluxes have less impact than surface heat fluxes on convection in both the Greenland and Labrador Sea and this result is insensitive to model resolution. is not robust across models. The mean strength of the Labrador Sea convection is important for the mean Atlantic Meridional Overturning Circulation (AMOC) and in around half of the models the variability of Labrador Sea convection is a significant contributor to the variability of the AMOC.