Observation and Parameterization of Ablation at the Base of Ronne Ice Shelf, Antarctica

By A. Jenkins, K. Nicholls, H. Corr. 2010

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Convection-Driven Melting near the Grounding Lines of Ice Shelves and Tidewater Glaciers (2011, methodology): “However, the weak dependence of the derived expressions on plume Reynolds number is unvalidated by geophysical-scale observations, and constant Stanton numbers appear to be at least as good a choice (McPhee 1992; McPhee et al. 1999; Jenkins et al. 2010).”
Modeling the impact of glacial runoff on fjord circulation and submarine melt rate using a new subgrid-scale parameterization for glacial plumes (2015, background): “Melt rate is strongly dependent on the velocity at the ice-ocean interface [Jenkins et al., 2010], and so cannot be properly predicted without knowledge of these currents (supporting information).”