Modeling ice shelf cavities in a z coordinate ocean general circulation model

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Modeling the impact of glacial runoff on fjord circulation and submarine melt rate using a new subgrid-scale parameterization for glacial plumes (2015, methodology): “The model has a nonhydrostatic capability that makes it suitable for the study of areas of complex bathymetry and buoyant upwellings and includes options to incorporate horizontal ice shelves [Losch, 2008] and vertical ice faces [Xu et al., 2012].”
Dynamically and Kinematically Consistent Global Ocean Circulation and Ice State Estimates (2013, background): “Recent, and as yet incomplete, model developments have been directed at determining the interactions of changing ocean temperatures and ice sheet response, and for the purpose of inclusion into the coupled state estimation system (Losch, 2008).”