Adaptation of an unstructured-mesh, finite-element ocean model to the simulation of ocean circulation beneath ice shelves

• Published in: Ocean modelling (Oxford) Vol. 67; pp. 39 - 51
• Main Authors: Kimura, Satoshi, Candy, Adam S., Holland, Paul R., Piggott, Matthew D., Jenkins, Adrian
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.07.2013
• Subjects: Fluidity-ICOM; Ice shelf; Ice–ocean interaction; Unstructured mesh; Ice shelf; Unstructured mesh; Ice–ocean interaction; Fluidity-ICOM
• ISSN: 1463-5003; 1463-5011
• DOI: 10.1016/j.ocemod.2013.03.004

•Ocean circulation beneath ice shelves is simulated using an unstructured-mesh.•We represent a smoothly varying ice base in the presence of a vertical ice front.•We implemented ice shelf/ocean interaction in the context of finite-element method. Several different classes of ocean model are capable of representing floating glacial ice shelves. We describe the incorporation of ice shelves into Fluidity-ICOM, a nonhydrostatic finite-element ocean model with the capacity to utilize meshes that are unstructured and adaptive in three dimensions. This geometric flexibility offers several advantages over previous approaches. The model represents melting and freezing on all ice-shelf surfaces including vertical faces, treats the ice shelf topography as continuous rather than stepped, and does not require any smoothing of the ice topography or any of the additional parameterisations of the ocean mixed layer used in isopycnal or z-coordinate models. The model can also represent a water column that decreases to zero thickness at the ‘grounding line’, where the floating ice shelf is joined to its tributary ice streams. The model is applied to idealised ice-shelf geometries in order to demonstrate these capabilities. In these simple experiments, arbitrarily coarsening the mesh outside the ice-shelf cavity has little effect on the ice-shelf melt rate, while the mesh resolution within the cavity is found to be highly influential. Smoothing the vertical ice front results in faster flow along the smoothed ice front, allowing greater exchange with the ocean than in simulations with a realistic ice front. A vanishing water-column thickness at the grounding line has little effect in the simulations studied. We also investigate the response of ice shelf basal melting to variations in deep water temperature in the presence of salt stratification.