Not exact matches
Sea
ice reflects most of the sun's energy, he explained, whereas the open ocean absorbs more energy, and thus the disappearance of sea
ice triggers even more warming, in a positive -
feedback loop called
albedo.
«If you can time your emissions so they have the least impact then you will not
trigger these very sensitive regions to start warming by this
ice albedo feedback process.»
«If you can time your emissions so they have the least impact then you will not
trigger these very sensitive regions to start warming by this
ice albedo feedback process.»
The main idea is that melting
triggers more melting through the
ice albedo feedback mechanism.
Re # 5 As far as I understand it (drawing on my recollections of a lecture Hansen gave here at Yale a few weeks back), the actual net forcing associated with Milankovich cycles is relatively small, but it tends to
trigger massive
feedbacks (e.g. polar
ice expanding, lowering
albedo, cooling, expanding more) that «snowball» into a glacial period.