Inclusion of ecologically based trait variation in plant functional types reduces the projected land carbon sink in an earth system model

Earth system models demonstrate large uncertainty in projected changes in terrestrial carbon budgets. The lack of inclusion of adaptive responses of vegetation communities to the environment has been suggested to hamper the ability of modeled vegetation to adequately respond to environmental change....

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Published inGlobal change biology Vol. 21; no. 8; pp. 3074 - 3086
Main Authors Verheijen, Lieneke M, Aerts, Rien, Brovkin, Victor, Cavender‐Bares, Jeannine, Cornelissen, Johannes H. C, Kattge, Jens, Bodegom, Peter M
Format Journal Article
LanguageEnglish
Published England Blackwell Science 01.08.2015
Blackwell Publishing Ltd
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Summary:Earth system models demonstrate large uncertainty in projected changes in terrestrial carbon budgets. The lack of inclusion of adaptive responses of vegetation communities to the environment has been suggested to hamper the ability of modeled vegetation to adequately respond to environmental change. In this study, variation in functional responses of vegetation has been added to an earth system model (ESM) based on ecological principles. The restriction of viable mean trait values of vegetation communities by the environment, called ‘habitat filtering’, is an important ecological assembly rule and allows for determination of global scale trait–environment relationships. These relationships were applied to model trait variation for different plant functional types (PFTs). For three leaf traits (specific leaf area, maximum carboxylation rate at 25 °C, and maximum electron transport rate at 25 °C), relationships with multiple environmental drivers, such as precipitation, temperature, radiation, and CO₂, were determined for the PFTs within the Max Planck Institute ESM. With these relationships, spatiotemporal variation in these formerly fixed traits in PFTs was modeled in global change projections (IPCC RCP8.5 scenario). Inclusion of this environment‐driven trait variation resulted in a strong reduction of the global carbon sink by at least 33% (2.1 Pg C yr⁻¹) from the 2nd quarter of the 21st century onward compared to the default model with fixed traits. In addition, the mid‐ and high latitudes became a stronger carbon sink and the tropics a stronger carbon source, caused by trait‐induced differences in productivity and relative respirational costs. These results point toward a reduction of the global carbon sink when including a more realistic representation of functional vegetation responses, implying more carbon will stay airborne, which could fuel further climate change.
Bibliography:http://dx.doi.org/10.1111/gcb.12871
istex:12E3BC445A5175A1D988A47D5A5E31513747F099
Theme Sustainable Earth Research - No. TKS09-03
Netherlands Organization for Scientific Research (NWO)
ArticleID:GCB12871
DIVERSITAS
GIS 'Climat, Environnement et Société' France
Data S1. Description of trait-environment relationships. Figure S1. Time-series of changes in global carbon pools. Figure S2. Time-series of changes in global mean carbon fluxes. Figure S3. Latitudinal gradients of PFT-averaged traits. Figure S4. Latitudinal gradients of mean annual heterotrophic respiration.
Global Land Project
IGBP
ark:/67375/WNG-WRS41R25-J
QUEST
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:1354-1013
1365-2486
DOI:10.1111/gcb.12871