Compensation Between Cloud Feedback and Aerosol-Cloud Interaction in CMIP6 Models

Chenggong Wang, Brian J. Soden, Wenchang Yang, Gabriel A. Vecchi

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37 Scopus citations


The most recent generation of climate models (the 6th Phase of the Coupled Model Intercomparison Project) yields estimates of effective climate sensitivity (ECS) that are much higher than past generations due to a stronger amplification from cloud feedback. If plausible, these models require substantially larger greenhouse gas reductions to meet global warming targets. We show that models with a more positive cloud feedback also have a stronger cooling effect from aerosol-cloud interactions. These two effects offset each other during the historical period when both aerosols and greenhouse gases increase, allowing either more positive or neutral cloud feedback models to reproduce the observed global-mean temperature change. Since anthropogenic aerosols primarily concentrate in the Northern Hemisphere, strong aerosol-cloud interaction models produce an interhemispheric asymmetric warming. We show that the observed warming asymmetry during the mid to late 20th century is more consistent with low ECS (weak aerosol indirect effect) models.

Original languageEnglish (US)
Article numbere2020GL091024
JournalGeophysical Research Letters
Issue number4
StatePublished - Feb 28 2021

All Science Journal Classification (ASJC) codes

  • Geophysics
  • General Earth and Planetary Sciences


  • CMIP6
  • aerosol-cloud interaction
  • climate sensitivity
  • cloud feedback
  • global warming


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