Abstract
In recent decades there has been increasing discussion of the possible effects of anthropogenic changes in climate. The biological consequences of anticipated changes have been discussed mostly in terms of ecosystem reaction to an increasingly warmer climate (Emanuel et al. 1985; Bonan et al. 1990; Botkin & Nisbet 1992; Chapin et al. 1995), involving a northward movement of boreal forest into areas currently covered by tundra (cf. Prentice et al. 1991). This generalized view can and needs to be discussed in depth in order to reach a more reliable prediction. This paper focuses on structural changes in time and space in the forest-tundra ecotone (i.e. the transition zone from closed forest to tundra, crossing the treeline up to the krummholz limit). The dynamic nature of the structural changes is discussed in relation to a hypothetical climate-vegetation equilibrium.
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Hofgaard, A. (1997). Structural changes in the forest-tundra ecotone:A dynamic process. In: Huntley, B., Cramer, W., Morgan, A.V., Prentice, H.C., Allen, J.R.M. (eds) Past and Future Rapid Environmental Changes. NATO ASI Series, vol 47. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-60599-4_20
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DOI: https://doi.org/10.1007/978-3-642-60599-4_20
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