Articles | Volume 26, issue 17
https://doi.org/10.5194/acp-26-12591-2026
https://doi.org/10.5194/acp-26-12591-2026
Research article
 | 
04 Sep 2026
Research article |  | 04 Sep 2026

Planetary albedo change exacerbates surface warming: a perspective from cloud-type changes

Ruixue Li, Jiming Li, Bida Jian, Lijie Zhang, and Jiayi Li

Data sets

orcing, Cloud Feedbacks, Cloud Masking, and Internal Variability in the Cloud Radiative Effect Satellite Record (Data) S. P. Raghuraman et al. https://doi.org/10.5281/zenodo.7623726

ERA5 monthly averaged data on pressure levels from 1940 to present H. Hersbach et al. https://doi.org/10.24381/cds.6860a573

ERA5 monthly averaged data on single levels from 1940 to present H. Hersbach et al. https://doi.org/10.24381/cds.f17050d7

MERRA-2 tavgM_2d_aer_Nx: 2d, monthly mean, time-averaged, single-level, assimilation, aerosol diagnostics V5.12.4 Global Modeling and Assimilation Office (GMAO) https://doi.org/10.5067/FH9A0MLJPC7N

CERES Energy Balanced and Filled (EBAF) Ed4.2.1 NASA/LARC/SD/ASDC https://ceres-tool.larc.nasa.gov/ord-tool/jsp/EBAF421Selection.jsp

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Short summary
Using satellite radiation observations and a surface energy framework, we show that recent cloud changes weakly affect global mean warming but strongly modulate regional warming, enhancing warming in low- and mid-latitudes while mitigating it in polar regions. This effect is driven by changes from low- and mid-level clouds to high-level thin clouds, reducing planetary albedo and weakening longwave emission, with distinct controls in the two hemispheres.
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