This example is an important step towards three-dimensional coupling. We'll sort out passing the latent heat from the ocean model to the ice in freezing or ice-covered areas, and passing the excess latent heat from the ice into the ocean when the ice disappears.
This task can be broken up into a few subtasks which I propose we complete in one PR:
thermally coupled ice-ocean simulation
thermally and salinity-coupled ice-ocean simulation
mechanically, thermally, and salinity coupled ice-ocean simulation
Once the third is finished then we have a viable coupled setup.
This example is an important step towards three-dimensional coupling. We'll sort out passing the latent heat from the ocean model to the ice in freezing or ice-covered areas, and passing the excess latent heat from the ice into the ocean when the ice disappears.
This task can be broken up into a few subtasks which I propose we complete in one PR:
Once the third is finished then we have a viable coupled setup.