Not exact matches
Virtually ice - free summers in the
arctic sea could well arrive by 2030, with troubling implications for accelerated
albedo feedback and possibly disruptive changes in the jet stream.
In the NH a lot of land surrounding the
arctic ocean is subject to the combination of decrease in seasonal snow cover (with climate warming), and decreasing
albedo due to vegetation
feedbacks.
Both these factors (as well as sea ice
albedo feedbacks, give the
arctic region very strong positive
feedback which regionally amplify the GW signal.
Apart
albedo, shouldn't we expect a classical water vapour
feedback (and so DLF forcing) as
arctic ice is melting and
arctic seas / ocean warming?
Subject of some specific concern about global warming because of large temperature rises predicted for the
arctic, and because of some
arctic - specific
feedback effects (e.g. the
albedo feedback following loss of
arctic sea ice).
Ice -
albedo feedback, he added, could give considerably greater warming in
arctic regions.
Hence, one gets a positive
feedback whereby the warming of the
arctic leads to ice melting which lowers the
albedo of the earth and thereby leads to further warming of the
arctic (and global climate system as a whole).
The increased
albedo from melting
arctic ice should not matter very much, but the newly exposed cold surface water might absorb extra carbon dioxide, acting as a negative
feedback on the whole system.