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Non-forested ecoregions were assigned SEP values of 0.0 for all tree species under contemporary climate based on the assumption that most area capable of supporting forest cover is currently occupied by trees or mountain shrubs (e.g., in recently disturbed areas) and these generally arid ecoregions have unsuitable climates for trees.
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Thus, we ran the model under historical fire and contemporary climate conditions until plant community composition reached a state of quasi-equilibrium (after ~600 years), and then verified that the resulting composition and distribution approximated contemporary landscape conditions (Additional file 4: Appendix 4).
Fig. 4 Species abundance over 90 years of continued contemporary climate compared to B1 and A2 climate change scenarios under suppressed, historical, and future fire regimes.
Pithan, F. & Mauritsen, T. Arctic amplification dominated by temperature feedbacks in contemporary climate models.
The ways in which water managers can adapt to contemporary climate variability, and which ultimately will serve as the foundation to adapting to climate change are described.
The presumptive targets of their argument are at least some of the modeling projects undertaken in contemporary climate science.
Contemporary climate change has two principal definitions.
Year 2000 conditions reflect 600 simulated years of contemporary climate and the historical fire regime.
Therefore, research, policy, and practice should accept contemporary climate change as one challenge amongst many within disaster risk reduction.
Year 2000 distributions reflect the landscape after 600 simulated years of contemporary climate and the historical fire regime.
Contemporary climate change is one more to add to this well-established list and it should be added to ensure that climate change vulnerability and resilience are addressed.
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