Cited by 93Ecosystem dynamics and resiliencePlant Water Relations and Carbon DynamicsClimate variability and models

Increasing atmospheric CO2 overrides the historical legacy of multiple stable biome states in Africa

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Moncrieff, Glenn R., Scheiter, Simon, Bond, William J., Higgins, Steven I.·2014·New Phytologist

Abstract

The dominant vegetation over much of the global land surface is not predetermined by contemporary climate, but also influenced by past environmental conditions. This confounds attempts to predict current and future biome distributions, because even a perfect model would project multiple possible biomes without knowledge of the historical vegetation state. Here we compare the distribution of tree- and grass-dominated biomes across Africa simulated using a dynamic global vegetation model (DGVM). We explicitly evaluate where and under what conditions multiple stable biome states are possible for current and projected future climates. Our simulation results show that multiple stable biomes states are possible for vast areas of tropical and subtropical Africa under current conditions. Widespread loss of the potential for multiple stable biomes states is projected in the 21st Century, driven by increasing atmospheric CO2 . Many sites where currently both tree-dominated and grass-dominated biomes are possible become deterministically tree-dominated. Regions with multiple stable biome states are widespread and require consideration when attempting to predict future vegetation changes. Testing for behaviour characteristic of systems with multiple stable equilibria, such as hysteresis and dependence on historical conditions, and the resulting uncertainty in simulated vegetation, will lead to improved projections of global change impacts.

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  • Increased levels of CO2 are reducing the stability of several biomes (notably savanna and grassland) and favoring the establishment of forests and denser vegetation.

    “Alternatively, increased levels of CO2 are reducing the stability of several biomes (notably savanna and grassland) and favoring the establishment of forests and denser vegetation [27,28].”

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Research works printed but not linked: 1

  1. Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL, eds. Climate change 2007: the physical science basis. Contribution of Working Group I to the fourth assessment report of the Intergovernmental Panel on climate change. Cambridge, UK & New York, NY, USA: Cambridge University Press.

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Authors
Moncrieff, G. R., Scheiter, S., Bond, W. J., & Higgins, S. I.
Affiliations
  • Goethe University Frankfurt (DE)
  • Senckenberg Research Institute and Natural History Museum Frankfurt/M (DE)
  • University of Cape Town (ZA)
  • University of Otago (NZ)
Corresponding author
Moncrieff, Glenn R.
Venue
New Phytologist
Publisher
Wiley
Published
2013-10-28
Volume
201
Issue
3
Pages
908-915
ISSN
  • 0028-646X (ISSN-L)
  • 1469-8137
OpenAlex
W2101461468
Cited by
93
References
72
Citations by year
2026: 1 · 2025: 9 · 2024: 6 · 2023: 3 · 2022: 5 · 2021: 7 · 2020: 6 · 2019: 6 · 2018: 11 · 2017: 7 · 2016: 13 · 2015: 14 · 2014: 5
FWCI
8.14
Type
journal article
Language
en
Open access
Locations
  • New Phytologist (publishedVersion)
  • PubMed (publishedVersion)
  • ERef Bayreuth (University of Bayreuth) (submittedVersion)
Funders
Deutscher Akademischer Austauschdienst
Topics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Ecosystem dynamics and resilience
  • Physical Sciences › Environmental Science › Global and Planetary Change › Plant Water Relations and Carbon Dynamics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
Keywords
atmospheric CO2 increase, dynamic global vegetation models, Africa, vegetation-climate interactions
MeSH terms
Africa, Atmosphere, Carbon Dioxide, Computer Simulation, Poaceae, Rain, Time Factors, Trees, Biota

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