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
kinimod on A High Schooler’s Take o… geoffbeacon on A High Schooler’s Take o… Bob Loblaw on Not Even Wrong? Bob Loblaw on Not Even Wrong? Tom Passin on Not Even Wrong? convictstreak on A High Schooler’s Take o… Bob Loblaw on Not Even Wrong? Cliff Mass on Not Even Wrong? jgnfld on Not Even Wrong? Bob Loblaw on Not Even Wrong? kinimod on A High Schooler’s Take o… jgnfld on Not Even Wrong? geoffbeacon on A High Schooler’s Take o… climatefreak on A High Schooler’s Take o… Lowlander on Not Even Wrong? -
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