Why is the Arctic interior arranged in steps, and how much heat do they let through?
Below the Arctic sea ice there is enough heat to melt all of it. A strong salinity stratification, with staircases in it, keeps the heat down.
Warm Atlantic water sits a few hundred metres below the ice. It is held there by a strong salinity stratification, and within that stratification the temperature and salinity profiles are arranged in staircases: well-mixed layers separated by sharp interfaces. Each interface limits the upward heat flux, and the turbulence inside the layers is double-diffusive. Whether these staircases survive as the Arctic warms and freshens is part of what determines how fast the ice feels the heat below it.
In my PhD I proposed a mechanism for how the staircases form, an instability that appears when double diffusion and stratified turbulence act together, and tested it with direct numerical simulations. I then looked at how much heat passes through a staircase when turbulence is added. What I would like to know now is what happens to them as the Arctic changes.