Causes of Higher Climate Sensitivity in CMIP6 Models
Lawrence Livermore National Laboratory · University of Leeds · +2 more institutions
Abstract
Abstract Equilibrium climate sensitivity, the global surface temperature response to CO doubling, has been persistently uncertain. Recent consensus places it likely within 1.5–4.5 K. Global climate models (GCMs), which attempt to represent all relevant physical processes, provide the most direct means of estimating climate sensitivity via CO quadrupling experiments. Here we show that the closely related effective climate sensitivity has increased substantially in Coupled Model Intercomparison Project phase 6 (CMIP6), with values spanning 1.8–5.6 K across 27 GCMs and exceeding 4.5 K in 10 of them. This (statistically insignificant) increase is primarily due to stronger positive cloud feedbacks from decreasing…
Citation impact
- FWCI
- 117.51
- Percentile
- 100%
- References
- 82
Authors
8- MDMark D. ZelinkaCorresponding
Lawrence Livermore National Laboratory
- TATimothy A. Myers
Lawrence Livermore National Laboratory
- DTDaniel T. McCoy
University of Leeds, National Centre for Atmospheric Science
- SPStephen Po–Chedley
Lawrence Livermore National Laboratory
- PCPeter Caldwell
Lawrence Livermore National Laboratory
Topics & keywords
- Coupled model intercomparison project
- Extratropical cyclone
- Climate sensitivity
- Climatology
- Climate model
- Cloud feedback
- Environmental science
- Cloud cover
- Climate action
Funding
- UDU.S. Department of EnergyAward: AC52-07NA27344
- ICImperial College London
- ECEuropean CommissionAward: 641727
- OOOffice of ScienceAward: DE-AC52-07NA27344
- LDLaboratory Directed Research and DevelopmentAward: DE-AC52-07NA27344
- LLLawrence Livermore National LaboratoryAwards: 18-ERD-054, DE-AC52-07NA27344, AC52-07NA27344