Abstract
Simulations of the land surface carbon cycle typically compress functional diversity into a small set of plant functional types (PFT), with parameters defined by the average value of measurements of functional traits. In most earth system models, all wild plant life is represented by between five and 14 PFTs and a typical grid cell (≈100 × 100 km) may contain a single PFT. Model logic applied to this coarse representation of ecological functional diversity provides a reasonable proxy for the carbon cycle, but does not capture the non-linear influence of functional traits on productivity. Here we show through simulations using the Energy Exascale Land Surface Model in 15 diverse terrestrial landscapes, that better accounting for functional diversity markedly alters predicted total carbon uptake. The shift in carbon uptake is as great as 30% and 10% in boreal and tropical regions, respectively, when compared to a single PFT parameterized with the trait means. The traits that best predict gross primary production vary based on vegetation phenology, which broadly determines where traits fall within the global distribution. Carbon uptake is more closely associated with specific leaf area for evergreen PFTs and the leaf carbon to nitrogen ratio in deciduous PFTs.
Original language | English |
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Article number | e2021JG006606 |
Pages (from-to) | 1-17 |
Number of pages | 17 |
Journal | Journal of Geophysical Research: Biogeosciences |
Volume | 127 |
Issue number | 3 |
Early online date | 6 Mar 2022 |
DOIs | |
Publication status | Published - Mar 2022 |
Bibliographical note
Funding Information:This research was supported as part of the Energy Exascale Earth System Model (E3SM) project funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research (including Grant DE-SC0012677 to P.B.R.), Biological Integration Institutes Grant NSF-DBI-2021898 (to P. B. Reich), and by NSF grants OAC-1934634 and IIS-1563950 (to A. Banerjee).
Funding Information:
This research was supported as part of the Energy Exascale Earth System Model (E3SM) project funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research (including Grant DE‐SC0012677 to P.B.R.), Biological Integration Institutes Grant NSF‐DBI‐2021898 (to P. B. Reich), and by NSF grants OAC‐1934634 and IIS‐1563950 (to A. Banerjee).
Publisher Copyright:
© 2022 The Authors.
Funding
This research was supported as part of the Energy Exascale Earth System Model (E3SM) project funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research (including Grant DE-SC0012677 to P.B.R.), Biological Integration Institutes Grant NSF-DBI-2021898 (to P. B. Reich), and by NSF grants OAC-1934634 and IIS-1563950 (to A. Banerjee). This research was supported as part of the Energy Exascale Earth System Model (E3SM) project funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research (including Grant DE‐SC0012677 to P.B.R.), Biological Integration Institutes Grant NSF‐DBI‐2021898 (to P. B. Reich), and by NSF grants OAC‐1934634 and IIS‐1563950 (to A. Banerjee).
Funders | Funder number |
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Biological Integration Institutes | OAC-1934634, NSF-DBI-2021898, IIS-1563950 |
U.S. Department of Energy | |
Office of Science | |
Biological and Environmental Research | OAC‐1934634, NSF‐DBI‐2021898, IIS‐1563950, DE‐SC0012677 |
Biological and Environmental Research |
Keywords
- carbon cycle
- diversity
- functional traits
- global models
- phenology