A hierarchical, multivariate meta-analysis approach to synthesising global change experiments

Kiona Ogle*, Yao Liu, Sara Vicca, Michael Bahn

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

10 Citations (Scopus)
18 Downloads (Pure)

Abstract

Meta-analyses enable synthesis of results from globally distributed experiments to draw general conclusions about the impacts of global change factors on ecosystem function. Traditional meta-analyses, however, are challenged by the complexity and diversity of experimental results. We illustrate how several key issues can be addressed via a multivariate, hierarchical Bayesian meta-analysis (MHBM) approach applied to information extracted from published studies.
We applied an MHBM to log-response ratios for aboveground biomass (AB, n = 300), belowground biomass (BB, n = 205), and soil CO2 exchange (SCE, n = 544), representing 100 studies. The MHBM accounted for study duration, climate effects, and covariation among the AB, BB, and SCE responses to elevated CO2 (eCO2) and/or warming.
The MHBM revealed significant among-study covariation in the AB and BB responses to experimental treatments. The MHBM imputed missing duration (4.2%) and climate (6%) data, and revealed that climate context governs how eCO2 and warming impact ecosystem function. Predictions identified biomes that may be particularly sensitive to eCO2 or warming, but that are under-represented in global change experiments.
The MHBM approach offers a flexible and powerful tool for synthesizing disparate experimental results reported across multiple studies, sites, and response variables.
Original languageEnglish
Pages (from-to)2382-2394
Number of pages13
JournalNew Phytologist
Volume231
Issue number6
Early online date13 Jul 2021
DOIs
Publication statusPublished - Sept 2021

Keywords

  • Bayesian meta-analysis
  • climate warming
  • elevated CO2
  • global change experiments
  • hierarchical model
  • incomplete reporting
  • multivariate meta-analysis
  • elevated CO

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