Using terrestrial laser scanning to constrain forest ecosystem structure and functions in the Ecosystem Demography model (ED2.2)

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  • Félicien Meunier
  • Sruthi M. Krishna Moorthy
  • Marc Peaucelle
  • Kim Calders
  • Louise Terryn
  • Verbruggen, Wim
  • Chang Liu
  • Ninni Saarinen
  • Niall Origo
  • Joanne Nightingale
  • Mathias Disney
  • Yadvinder Malhi
  • Hans Verbeeck

Terrestrial biosphere models (TBMs) are invaluable tools for studying plant-atmosphere interactions at multiple spatial and temporal scales, as well as how global change impacts ecosystems. Yet, TBM projections suffer from large uncertainties that limit their usefulness. Forest structure drives a significant part of TBM uncertainty as it regulates key processes such as the transfer of carbon, energy, and water between the land and the atmosphere, but it remains challenging to observe and reliably represent. The poor representation of forest structure in TBMs might actually result in simulations that reproduce observed land fluxes but fail to capture carbon pools, forest composition, and demography. Recent advances in terrestrial laser scanning (TLS) offer new opportunities to capture the three-dimensional structure of the ecosystem and to transfer this information to TBMs in order to increase their accuracy. In this study, we quantified the impacts of prescribing initial conditions (tree size distribution), constraining key model parameters with observations, as well as imposing structural observations of individual trees (namely tree height, leaf area, woody biomass, and crown area) derived from TLS on the state-of-the-art Ecosystem Demography model (ED2.2) of a temperate forest site (Wytham Woods, UK). We assessed the relative contributions of initial conditions, model structure, and parameters to the overall output uncertainty by running ensemble simulations with multiple model configurations. We show that forest demography and ecosystem functions as modelled by ED2.2 are sensitive to the imposed initial state, the model parameters, and the choice of key model processes. In particular, we show that: Parameter uncertainty drove the overall model uncertainty, with a mean contribution of 63ĝ€¯% to the overall variance of simulated gross primary production. Model uncertainty in the gross primary production was reduced fourfold when both TLS and trait data were integrated into the model configuration. Land fluxes and ecosystem composition could be simultaneously and accurately simulated with physically realistic parameters when appropriate constraints were applied to critical parameters and processes. We conclude that integrating TLS data can inform TBMs of the most adequate model structure, constrain critical parameters, and prescribe representative initial conditions. Our study also confirms the need for simultaneous observations of plant traits, structure, and state variables if we seek to improve the robustness of TBMs and reduce their overall uncertainties.

OriginalsprogEngelsk
TidsskriftGeoscientific Model Development
Vol/bind15
Udgave nummer12
Sider (fra-til)4783-4803
Antal sider21
ISSN1991-959X
DOI
StatusUdgivet - 2022

Bibliografisk note

Funding Information:
Acknowledgements. This research was funded by BELSPO (Belgian Science Policy Office) in the framework of the STEREO III programme – project 3D-FOREST (SR/02/355). The computational resources and services used in this work were provided by the VSC (Flemish Supercomputer Center), funded by the Research Foundation – Flanders (FWO) and the Flemish Government – EWI Department. During the preparation of this manuscript, Félicien Meunier was funded by the FWO as a junior postdoc and is thankful to this organisation for its financial support (FWO grant no. 1214720N). Ninni Saarinen was funded by the Academy of Finland (project number 315079). Kim Calders was funded by the European Union’s Horizon 2020 research and innovation programme under Marie Sklodowska-Curie grant no. 835398. Marc Peaucelle was funded by the FWO (grant no. G018319N) and the European Union’s Horizon 2020 research and innovation programme under Marie Sklodowska-Curie grant no. 891369. The TLS fieldwork was funded through the Metrology for Earth Observation and Climate project (MetEOC-2), grant number ENV55, within the European Metrology Research Programme (EMRP). The EMRP is jointly funded by the EMRP participating countries within EURAMET and the European Union. Funds for used for the purchase of the UCL RIEGL VZ-400 instrument were provided by the UK NERC National Centre for Earth Observation (NCEO). The census of the forest plot was supported by an ERC Advanced Investigator Grant to Yadvinder Malhi (GEM-TRAIT, grant number 321131). We are grateful to the whole PEcAn group and the ED2 team for helpful discussions and support related to the functioning of PEcAn and ED2.

Funding Information:
Financial support. This research has been supported by the Bel-

Publisher Copyright:
© 2022 Félicien Meunier et al.

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