Polar amplification

From Wikipedia, the free encyclopedia
Jump to: navigation, search

Polar amplification is the greater temperature increases in the Arctic compared to the earth as a whole as a result of the effect of feedbacks and other processes[1] It is not observed in the Antarctic, largely because the Southern Ocean acts as a heat sink and the lack of seasonal snow cover.[2] It is common to see it stated that "Climate models generally predict amplified warming in polar regions", e.g. Doran et al.[3]. However, climate models predict amplified warming for the Arctic but only modest warming for Antarctica.[2]

[edit] See also

[edit] References

  1. ^ Arctic Climate Impact Assessment - International Arctic Science Committee
  2. ^ a b "Antarctic cooling, global warming?". RealClimate. 3 December 2004. http://www.realclimate.org/index.php?p=18. 
  3. ^ Doran, Peter T.; Priscu, John C.; Lyons, W. Berry; Walsh, John E.; Fountain, Andrew G.; McKnight, Diane M.; Moorhead, DL; Virginia, RA et al. (31 January 2002). "Antarctic climate cooling and terrestrial ecosystem response". Nature 415 (6871): 517–20. doi:10.1038/nature710. PMID 11793010. http://www.nature.com/nature/journal/v415/n6871/full/nature710.html. 
Personal tools
Namespaces
Variants
Actions
Navigation
Interaction
Toolbox
Print/export