Abstract
Boreal forests of northern hemisphere are considered to be the major carbon sink in the world, and are potentially affecting carbon balance at large geographical scales (Kasischke and Stocks 2000; Schimel et al. 2001). This biome may be affected by warming air temperature, as the northern latitudes are where the effect of global warming is likely to be felt most strongly in the next several decades (Solomon et al. 2007). Therefore, better understanding of the patterns of forest development is relevant today, with respect to carbon sequestration of the ecosystems (Wirth et al. 2002).
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Osawa, A., Kajimoto, T. (2010). Development of Stand Structure in Larch Forests. In: Osawa, A., Zyryanova, O., Matsuura, Y., Kajimoto, T., Wein, R. (eds) Permafrost Ecosystems. Ecological Studies, vol 209. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-9693-8_7
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