Parameterizing the fresh-water flux from land ice to ocean with interactive icebergs in a coupled climate model

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OMIP contribution to CMIP6: experimental and diagnostic protocol for the physical component of the Ocean Model Intercomparison Project (2016, background): “This inconsistency is motivated by the desire to have the model ocean heat content related directly to the model prognostic temperature field, with that temperature field time stepped 20 according to conserved budget equations. Turning this inconsistency into an opportunity, McDougall (2003) noted t”
The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features (2019, methodology): “In the CM4 and ESM4 607 coupled models, frozen water from the land model component is handled by an iceberg 608 model which is part of the sea ice component as described in Martin and Adcroft [2010]. 609 We use updates to rolling and melting parameterizations described in Stern et al.”
Challenges and Prospects in Ocean Circulation Models (2019, background): “Martin and Adcroft (2010) make the icebergs an integral part of the hydrologic cycle in a fully coupled model.”