- #36
stuartmacg
- 28
- 6
Uncovering previously protected sea should allow a bit of radiative heat loss that was not there before, in addition of course to the gain from the absorption of polar sunlight over the same area.
Since the cold polar regions are warmed by fluid transfer from the rest of the globe, they will be above local radiative equilibrium with their polar skies. I would thus expect any increase in thermal connection (reduction in albedo) to increase the heat flow in both directions, increasing the existing net radiative outflow from these regions.
Since the cold polar regions are warmed by fluid transfer from the rest of the globe, they will be above local radiative equilibrium with their polar skies. I would thus expect any increase in thermal connection (reduction in albedo) to increase the heat flow in both directions, increasing the existing net radiative outflow from these regions.