Schuur, E.; Abbott, B.; Bowden, W.; Brovkin, V.; Camill, P. - In: Climatic Change 119 (2013) 2, pp. 359-374
Approximately 1700 Pg of soil carbon (C) are stored in the northern circumpolar permafrost zone, more than twice as much C than in the atmosphere. The overall amount, rate, and form of C released to the atmosphere in a warmer world will influence the strength of the permafrost C feedback to...
