13 May 2020
13 May 2020
Status: this preprint was under review for the journal OS but the revision was not accepted.

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

Torben Koenigk1,2, Ramon Fuentes-Franco1, Virna Meccia3, Oliver Gutjahr4, Laura C. Jackson5, Adrian L. New6, Pablo Ortega7, Christopher Roberts8, Malcolm Roberts5, Thomas Arsouze7, Doroteaciro Iovino9, Marie-Pierre Moine10, and Dmitry V. Sein11 Torben Koenigk et al.
  • 1Rossby Centre, Swedish Meteorological and Hydrological Institute, Norrköping, Sweden
  • 2Bolin Centre for Climate Research, Stockholm University, Sweden
  • 3Istituto di Scienze dell'Atmosfera e del Clima (CNR-ISAC), Bologna, Italy
  • 4Max Planck Institute for Meteorology, Hamburg, Germany
  • 5Met Office, Exeter EX1 3PB, UK
  • 6The National Oceanography Centre Southampton, UK
  • 7Barcelona Supercomputing Center – Centro Nacional de Supercomputación (BSC), Barcelona, Spain
  • 8European Centre for Medium-Range Weather Forecasts (ECMWF), Reading, UK
  • 9Fondazione Centro Euro-Mediterraneo sui Cambiamenti Climatici (CMCC), Bologna, Italy
  • 10CERFACS/CNRS, Toulouse, France
  • 11Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany

Abstract. 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.

Torben Koenigk et al.

Status: closed
Status: closed
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Torben Koenigk et al.

Torben Koenigk et al.


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Short summary
The mixing of water masses into the deep ocean in the North Atlantic is important for the entire global ocean circulation. We use seven global climate models to investigate the effect of increasing the model resolution on this deep ocean mixing. The main result is that increased model resolution leads to a deeper mixing of water masses in the Labrador Sea but has less effect in the Greenland Sea. However, most of the models overestimate the deep ocean mixing compared to observations.