Abstract
The boreal forest biome occupies 13 × 106km2. It comprises approximately 25% of the world’s forest land (Olson et al. 1983; Apps et al. 1993) and includes 2.6 × 106 km2 of peatlands (Gorham 1991). Changes in the extent or functioning of the boreal forest could substantially modify global climate through (1) release of its large stocks of soil carbon (Post et al. 1982; Kurz and Apps 1995), (2) changes in methane fluxes from peatlands (Reeburgh and Whalen 1992; Roulet and Ash 1992), or (3) changes in winter albedo and regional energy exchange (Bonan et al. 1992; Thomas and Rowntree 1992). Boreal forests have also been implicated as the “missing sink” for atmospheric carbon dioxide (Ciais et al. 1995). For these reasons, there has been considerable interest and speculation about future changes in the extent, structure, and functioning of the boreal forest.
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Chapin, F.S., Danell, K. (2001). Boreal Forest. In: Chapin, F.S., Sala, O.E., Huber-Sannwald, E. (eds) Global Biodiversity in a Changing Environment. Ecological Studies, vol 152. Springer, New York, NY. https://doi.org/10.1007/978-1-4613-0157-8_6
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