4.7 Article

Inferring future warming in the Arctic from the observed global warming trend and CMIP6 simulations

期刊

ADVANCES IN CLIMATE CHANGE RESEARCH
卷 12, 期 4, 页码 499-507

出版社

SCIENCE PRESS
DOI: 10.1016/j.accre.2021.04.002

关键词

CMIP6; Arctic warming projection; Global warming; Observational constraint

资金

  1. National Key R&D Program of China [2019YFA0607000]
  2. National Natural Science Foundation of China [41805050, 42075028, 41922044, 42088101, 41722502, 41521004]
  3. High-Performance Grid Computing Platform of Sun Yatsen University
  4. China National Supercomputer Center in Guangzhou

向作者/读者索取更多资源

The emergent constraint approach uses multi-model ensembles to link current/past climate variability to future climate changes, reducing uncertainty in multi-model projections. CMIP6 models show stronger Arctic warming but with larger spread, with projections positively correlated to simulated global warming trends during 1981-2011. Using observed global warming during the instrumental era can provide tighter constraints on future Arctic warming.
The emergent constraint approach is a way of using multi-model ensembles to identify the linkage between current/past climate variability and future climate changes, which has been widely used for narrowing down the uncertainty of multi-model projections of future climate change. Climate models of the latest Coupled Model Intercomparison Project Phase 6 (CMIP6) show a much stronger Arctic warming signal but with a larger inter-model spread. In this study, we find that the projected Arctic warming made by multi-models in CMIP6 is positively correlated with the simulated global warming trend during the period of 1981-2011 in historical runs. This enables us to tighter constraints to future warming in the Arctic by using the observed global warming during the instrument era. The fact that CMIP6 models tend to overestimate the trend of global mean surface temperature during 1981-2011, therefore, would imply a relative weak Arctic warming compared to the CMIP6 median warming projection.

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