Projected future climatic forcing on the global distribution of vegetation types

Author:

Allen Bethany J.12ORCID,Hill Daniel J.3ORCID,Burke Ariane M.4ORCID,Clark Michael567ORCID,Marchant Robert8ORCID,Stringer Lindsay C.8910ORCID,Williams David R.3ORCID,Lyon Christopher89ORCID

Affiliation:

1. Department of Biosystems Science and Engineering, ETH Zurich, Basel 4056, Switzerland

2. Computational Evolution Group, Swiss Institute of Bioinformatics, Lausanne 1015, Switzerland

3. School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK

4. Département d'Anthropologie, Université de Montréal, Montréal, Quebec, H3C 3J7, Canada

5. Smith School of Enterprise and the Environment, University of Oxford, Oxford, OX1 3QY, UK

6. Oxford Martin School, University of Oxford, Oxford, OX1 3BD, UK

7. Department of Biology, University of Oxford, Oxford, OX1 3RB, UK

8. Department of Environment and Geography, University of York, York, YO10 5NG, UK

9. Leverhulme Centre for Anthropocene Biodiversity, University of York, York, YO10 5DD, UK

10. York Environmental Sustainability Institute, University of York, York, YO10 5DD, UK

Abstract

Most emissions scenarios suggest temperature and precipitation regimes will change dramatically across the globe over the next 500 years. These changes will have large impacts on the biosphere, with species forced to migrate to follow their preferred environmental conditions, therefore moving and fragmenting ecosystems. However, most projections of the impacts of climate change only reach 2100, limiting our understanding of the temporal scope of climate impacts, and potentially impeding suitable adaptive action. To address this data gap, we model future climate change every 20 years from 2000 to 2500 CE, under different CO 2 emissions scenarios, using a general circulation model. We then apply a biome model to these modelled climate futures, to investigate shifts in climatic forcing on vegetation worldwide, the feasibility of the migration required to enact these modelled vegetation changes, and potential overlap with human land use based on modern-day anthromes. Under a business-as-usual scenario, up to 40% of terrestrial area is expected to be suited to a different biome by 2500. Cold-adapted biomes, particularly boreal forest and dry tundra, are predicted to experience the greatest losses of suitable area. Without mitigation, these changes could have severe consequences both for global biodiversity and the provision of ecosystem services. This article is part of the theme issue ‘Ecological novelty and planetary stewardship: biodiversity dynamics in a transforming biosphere’.

Funder

Eidgenössische Technische Hochschule Zürich

Leverhulme Trust

White Rose University Consortium

Publisher

The Royal Society

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