Equilibrium Climate Sensitivity
Equilibrium Climate Sensitivity is a climate metric defined as the equilibrium change in global mean surface temperature resulting from a doubling of atmospheric CO₂ concentration relative to pre-industrial levels, representing the long-term temperature response after the climate system has fully adjusted to the radiative forcing.
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Causes of Higher Climate Sensitivity in CMIP6 Models
Mark D. Zelinka, Timothy A. Myers, Daniel T. McCoy et al. · Geophysical Research Letters · 2020 · 1.8K citations · Full text
The Canadian Earth System Model version 5 (CanESM5.0.3)
Neil C. Swart, Jason N. S. Cole, Viatcheslav Kharin et al. · Geoscientific model development · 2019 · 1.3K citations · Full text
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Lawrence Livermore National Laboratory, United States
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NSF National Center for Atmospheric Research
Boulder, United States
33 h-index
126 publications
21.5K citations
University of Washington
Seattle, United States
22 h-index
39 publications
3.7K citations
Met Office
Exeter, United Kingdom
22 h-index
38 publications
7K citations
Max Planck Institute for Meteorology
Hamburg, Germany
22 h-index
55 publications
4.6K citations

Lawrence Livermore National Laboratory
Livermore, United States
19 h-index
95 publications
22.5K citations
University of Reading
Reading, United Kingdom
16 h-index
23 publications
3.5K citations

Stockholm University
Stockholm, Sweden
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29 publications
1.7K citations
NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
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48 publications
6.2K citations
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JAMES · 14 publications · 3.1K citations
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JGR · 10 publications · 970 citations
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