Various processes, including albedo change (the change in reflectivity when ice and snow are replaced by open land or ocean), amplify the warming which is observed in the Arctic. Yet the situation is complicated. Cloud cover can change, which also affects reflectivity and can reduce or increase Arctic warming. Atmospheric patterns can likewise change, as can the state of the atmosphere in general. Overall, although we know that the Arctic is warming faster than the planet as a whole, how great this amplification will be in the future remains uncertain.
Support Your Global Climate Blog
Recent Comments
Gerald Alldredge on Heat Waves b fagan on Heat Waves Susan Anderson on Heat Waves jgnfld on Heat Waves russellseitz on Heat Waves Glen Koehler on Heat Waves Dan Neuman on How Fast? Richard Rathbone on How Fast? michael Sweet on How Fast? Mal Adapted on How Hot? Mitch on How Fast? jgnfld on How Fast? jgnfld on How Fast? jgnfld on How Hot? bartoszkopras on How Fast? -
Recent Posts
Buy the book
astronomy
Blogroll
Global Warming
- Climate Change
- ClimateSight
- Goddard Institute for Space Studies
- GreenFyre’s
- Hadley Center for Climate Change
- History of Global Warming (Spencer Weart)
- IPCC (Intergovernmental Panel on Climate Change)
- James’s Empty Blog
- Maribo
- Old Man in a Cave
- Open Mind Archive on Skeptical Science
- Rabett Run
- RealClimate
mathematics

