Environmental Research Letters (Jan 2022)

Contrasting ecosystem constraints on seasonal terrestrial CO2 and mean surface air temperature causality projections by the end of the 21st century

  • Daniel F T Hagan,
  • Han A J Dolman,
  • Guojie Wang,
  • Kenny T C Lim Kam Sian,
  • Kun Yang,
  • Waheed Ullah,
  • Runping Shen

DOI
https://doi.org/10.1088/1748-9326/aca551
Journal volume & issue
Vol. 17, no. 12
p. 124019

Abstract

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Two centuries of studies have demonstrated the importance of understanding the interaction between air temperature and carbon dioxide (CO _2 ) emissions, which can impact the climate system and human life in various ways, and across different timescales. While historical interactions have been consistently studied, the nature of future interactions and the impacts of confounding factors still require more investigation in keeping with the continuous updates of climate projections to the end of the 21st century. Phase 6 of the Coupled Model Intercomparison Project (CMIP6), like its earlier projects, provides ScenarioMIP multi-model projections to assess the climate under different radiative forcings ranging from a low-end (SSP1–2.6) to a high-end (SSP5–8.5) pathway. In this study, we analyze the localized causal structure of CO _2, and near-surface mean air temperature (meanT) interaction for four scenarios from three CMIP6 models using a rigorous multivariate information flow (IF) causality, which can separate the cause from the effect within the interaction (CO _2 –meanT and meanT–CO _2 ) by measuring the rate of IF between parameters. First, we obtain patterns of the CO _2 and meanT causal structures over space and time. We found a contrasting emission-based impact of soil moisture (SM) and vegetation (leaf area index (LAI)) changes on the meanT–CO _2 causal patterns. That is, SM influenced CO _2 sink regions in SSP1–2.6 and source regions in SSP5–8.5, and vice versa found for LAI influences. On the other hand, they function similarly to constrain the future CO _2 impact on meanT. These findings are essential for improving long-term predictability where climate models might be limited.

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