Joel Wright
EF5
As far as the urban heat island effect goes, just how substantial is this difference, say a few hundred feet above the surface and upward? Obviously heat rises, so there would likely be some of this "extra heat" rising upward into the column. However, as it rises, wouldn't it begin to dissipate somewhat, and become more consistant with the outlying ambient airmass? Just how deep into the atmosphere is this heat island effect?