Cloud feedback uncertainty in the equatorial Pacific across CMIP6 models

Cloud feedback is the largest uncertainty in estimating Equilibrium Climate Sensitivity. In this study we focus on the equatorial Pacific, where CMIP6 model cloud feedback spread is notably large. Cloud radiative effects in this region are relevant fo

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Published
2025-10-10
DOI
https://doi.org/10.22541/essoar.172800386.60900932/v3
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
0.00

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article

Cloud feedback uncertainty in the equatorial Pacific across CMIP6 models

Peter Hill, Mark D. Zelinka, D Finney
Climate variability and models
article

Cloud feedback uncertainty in the equatorial Pacific across CMIP6 models

Peter Hill, Mark D. Zelinka, D Finney
article en

Abstract

Cloud feedback is the largest uncertainty in estimating Equilibrium Climate Sensitivity. In this study we focus on the equatorial Pacific, where CMIP6 model cloud feedback spread is notably large. Cloud radiative effects in this region are relevant fo

Lawrence Livermore National Laboratory (US), University of Leeds (GB), University of Reading (GB)
U.S. Department of Energy, Natural Environment Research Council, Lawrence Livermore National Laboratory
Openalex Percentile: Top 73%
Climate variability and models
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Cloud feedback uncertainty in the equatorial Pacific across CMIP6 models — Peter Hill, Mark D. Zelinka, et al. · (2025) | TGRS Research Map | TGRS