Impacts of trait variation through observed trait–climate relationships on performance of an Earth system model: a conceptual analysis

• Main Authors: L. M. Verheijen, V. Brovkin, R. Aerts, G. Bönisch, J. H. C. Cornelissen, J. Kattge, P. B. Reich, I. J. Wright, P. M. van Bodegom
• Format: Article
• Language: English
• Published: Copernicus Publications 2013-08-01
• Series: Biogeosciences
• Online Access: http://www.biogeosciences.net/10/5497/2013/bg-10-5497-2013.pdf

In many current dynamic global vegetation models (DGVMs), including those incorporated into Earth system models (ESMs), terrestrial vegetation is represented by a small number of plant functional types (PFTs), each with fixed properties irrespective of their predicted occurrence. This contrasts with natural vegetation, in which many plant traits vary systematically along geographic and environmental gradients. In the JSBACH DGVM, which is part of the MPI-ESM, we allowed three traits (specific leaf area (SLA), maximum carboxylation rate at 25 °C (Vcmax₂₅) and maximum electron transport rate at 25 °C (Jmax₂₅)) to vary within PFTs via trait–climate relationships based on a large trait database. The <i>R</i>²_adjusted of these relationships were up to 0.83 and 0.71 for Vcmax₂₅ and Jmax₂₅, respectively. For SLA, more variance remained unexplained, with a maximum <i>R</i>²_adjusted of 0.40. Compared to the default simulation, allowing trait variation within PFTs resulted in gross primary productivity differences of up to 50% in the tropics, in > 35% different dominant vegetation cover, and a closer match with a natural vegetation map. The discrepancy between default trait values and natural trait variation, combined with the substantial changes in simulated vegetation properties, together emphasize that incorporating climate-driven trait variation, calibrated on observational data and based on ecological concepts, allows more variation in vegetation responses in DGVMs and as such is likely to enable more reliable projections in unknown climates.