Forget ice, substitute snow - snow is ice of course.
The argument Stephen puts forward here is not nonsense. If the winter season lasts longer in the Northern Hemishere with more extensive snow cover, then, heat lost from the global system will be more than recent times have experienced. And compared to the Arctic these temperate regions will indeed have a greater affect on albedo losses, for the simple reason of a higher heat input of the sun, in these regions, being reflected back into space - heat input into the Arctic being relatively negligible for much of the year.
And, the point here is that the extent of and extended winter season in the temperate regions, is strongly connected to the the mean position of the jet stream.
I'm sure you can work it out.
Originally Posted by: Gandalf The White