Articles | Volume 10, issue 7
Geosci. Model Dev., 10, 2849–2874, 2017

Special issue: Nucleus for European Modelling of the Ocean - NEMO

Geosci. Model Dev., 10, 2849–2874, 2017

Development and technical paper 26 Jul 2017

Development and technical paper | 26 Jul 2017

Explicit representation and parametrised impacts of under ice shelf seas in the z coordinate ocean model NEMO 3.6

Pierre Mathiot1,2, Adrian Jenkins1, Christopher Harris2, and Gurvan Madec3 Pierre Mathiot et al.
  • 1British Antarctic Survey, Natural Environment Research Council, Cambridge, UK
  • 2Met Office, Exeter, UK
  • 3Sorbonne Universités (University Pierre et Marie Curie Paris 6)-CNRS-IRD-MNHN, LOCEAN Laboratory, Paris, France

Abstract. Ice-shelf–ocean interactions are a major source of freshwater on the Antarctic continental shelf and have a strong impact on ocean properties, ocean circulation and sea ice. However, climate models based on the ocean–sea ice model NEMO (Nucleus for European Modelling of the Ocean) currently do not include these interactions in any detail. The capability of explicitly simulating the circulation beneath ice shelves is introduced in the non-linear free surface model NEMO. Its implementation into the NEMO framework and its assessment in an idealised and realistic circum-Antarctic configuration is described in this study.

Compared with the current prescription of ice shelf melting (i.e. at the surface), inclusion of open sub-ice-shelf cavities leads to a decrease in sea ice thickness along the coast, a weakening of the ocean stratification on the shelf, a decrease in salinity of high-salinity shelf water on the Ross and Weddell sea shelves and an increase in the strength of the gyres that circulate within the over-deepened basins on the West Antarctic continental shelf. Mimicking the overturning circulation under the ice shelves by introducing a prescribed meltwater flux over the depth range of the ice shelf base, rather than at the surface, is also assessed. It yields similar improvements in the simulated ocean properties and circulation over the Antarctic continental shelf to those from the explicit ice shelf cavity representation. With the ice shelf cavities opened, the widely used three equation ice shelf melting formulation, which enables an interactive computation of melting, is tested. Comparison with observational estimates of ice shelf melting indicates realistic results for most ice shelves. However, melting rates for the Amery, Getz and George VI ice shelves are considerably overestimated.