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Diagnosing Linearity Along the Carbon Cascade in Terrestrial Biosphere Models and Observations

  • Huanyuan Zhang-Zheng
  • , Vivek K. Arora
  • , Peter Anthoni
  • , Thomas A.M. Pugh
  • , Atul K. Jain
  • , Wenping Yuan
  • , Yadvinder Malhi
  • , Julia Nabel
  • , Daniel S. Goll
  • , Julia Pongratz
  • , Benjamin Poulter
  • , Anthony P. Walker
  • , Sönke Zaehle
  • , Jürgen Knauer
  • , Etsushi Kato
  • , Ruijie Ding
  • , Minxue Tang
  • , Stephen Sitch
  • , Michael O'Sullivan
  • , César Terrer
  • Hanqin Tian, Naiqing Pan, Pierre Friedlingstein, Akihiko Ito, Qing Sun, Jeanne Decayeux, Benjamin D. Stocker

Research output: Contribution to journal › Article › peer-review

Abstract

Elevated carbon dioxide (eCO2) acts as a fertiliser for photosynthesis, driving an increase in gross primary production (GPP). However, it is unclear how effectively increased GPP propagates along the ‘carbon (C) cascade’ to increase net primary production (NPP) and vegetation C stocks (Cveg) in different plant compartments. Vegetation models were criticised for being overly sensitive to photosynthesis (source-driven), neglecting sink-driven processes which may attenuate (or amplify) changes in NPP and vegetation C stocks. Here, we introduce an analytical framework to diagnose linearity (L) as ratios of relative changes in linked fluxes and pools. We then apply this framework to 16 models of the TRENDY v11 ensemble and to observation-based estimates of CO2 sensitivities. We found widely varying global patterns in L across models. Six models showed a majority of grid cells with larger relative changes in NPP than in GPP (LNPP:GPP > 1 for > 60% of gridcells), indicating increased vegetation carbon use efficiency under eCO2. Only three models had LNPP:GPP < 1 for > 60% of gridcells. Four models showed a majority of gridcells with larger relative changes in estimated steady-state Cveg than in NPP, while five models showed the opposite—in both cases with a large spread of LCveg*:NPP across grid cells within models. Observations-based analysis reveals median LCveg*:NPP < 1 overall but evidence is insufficient for a conclusion. Three models showed a larger relative increase in root C than in Cveg, (LCroot:Cveg > 1) while five models showed the opposite. Most field evidence shows LCroot:Cveg > 1. Widely differing distributions of L among models and links in the C cascade reveal a strong influence of nonlinear behaviour in individual models. However, due to the spread in L, across the whole models ensemble, L deviations from 1 were roughly balanced, leading to an overall linear behaviour of terrestrial C cycle representations in the multi-model-mean.

Original languageEnglish
Article numbere70982
JournalGlobal Change Biology
Volume32
Issue number7
DOIs
StatePublished - Jul 2026

Funding

This work was supported by the U.S. Department of Energy, Next Generation Ecosystem Experiments-Tropics, Swiss National Science Foundation (Grant PCEFP2_181115) and Swedish research council for sustainable development (Grant 2023-00361). H.Z.-Z. was supported as part of the Next Generation Ecosystem Experiments-Tropics, funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research. JSBACH simulations are performed using resources of the Deutsches Klimarechenzentrum (DKRZ) granted by its Scientific Steering Committee (WLA) under project 891. A.I. was supported by JSPS KAKENHI (grant no. 21H05318). Q.S. was supported by the Swiss National Science Foundation (200020 200511). Simulations of LPX-Bern were performed on UBELIX (https://www.id.unibe.ch/hpc), the HPC cluster at the University of Bern. T.A.M.P. was funded under the European Union‘s Horizon 2020 programme (grant agreement no. 758873, TreeMort) and Horizon Europe (101141836, Tree2Globe). This study is a contribution to the Swedish government‘s strategic research areas BECC and MERGE and the Nature-based Future Solutions profile area at Lund University. This study is supported by Swedish research council for sustainable development (grant: 2023-00361). ORNL is managed by UT-Battelle LLC, for the DOE under contract DE-AC05-1008 00OR22725. B.D.S. acknowledges funding from the Swiss National Science Foundation grant PCEFP2_181115. J.K. acknowledges support from the UTS Chancellor‘s Research Fellowship. Open access publishing facilitated by Universitat Bern, as part of the Wiley - Universitat Bern agreement via the Consortium Of Swiss Academic Libraries.

Keywords

  • carbon allocation
  • carbon cycle
  • elevated CO
  • gross primary production
  • net primary production
  • vegetation models

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