Abstract
AbstractAimTree species may be vulnerable to migration lags because they are sessile, long‐lived, have a small intrinsic growth rate and relatively short dispersal. Our study assesses if those ecological mechanisms will mitigate the progression of the north‐eastern American temperate forest leading edge into the boreal forest.LocationThe North‐eastern boreal‐temperate forest ecotone (from 43° to 51° North and 80° to 60° West).TaxonOur approach involved 15 forest species classified into four representative forest communities of the eastern boreal‐temperate forest.MethodsWe performed simulations on the boreal‐temperate ecotone using a state and transition model (STM), wherein forest communities are classified in four states: boreal, temperate, mixed and stands in regeneration. We propose a new modelling approach based on metapopulation theory to account for dispersal limitations and the demography of the temperate and boreal forests. We calibrated the STM model with an extensive dataset of 48,940 forest inventory plots. We projected the boreal‐temperate forest landscape over 23 General Circulation models (GCMs) from the RCP 8.5 emission scenario to study the forest communities dynamics at the landscape scale under climate change.ResultsSimulations of climate changes predict a significant increase of temperate forest dominance within the ecotone, mainly due to the conversion of mixed stands into temperate stands. The leading edge of the temperate forest will however move only 304 m in latitude (95% CI: 0.18–0.56) into the boreal forest by the end of this century. In comparison, the average expansion rate was 2,555 m/year (95% CI: 1,969–2,932) when we released the dispersal constraint and even higher with an average rate of 7,197 m/year (95% CI: 5,722–9,776) when we released the dispersal and demography constraints.Main conclusionsThe northern edge of the temperate forest distribution does not change with almost no movement toward the north for either temperate or mixed communities by the end of this century. Slow demographic and dispersal rates prevent any substantial movement in temperate forests, with much faster migration rates when these constraints are removed.
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