Articles | Volume 24, issue 12
https://doi.org/10.5194/acp-24-7331-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-24-7331-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
General circulation models simulate negative liquid water path–droplet number correlations, but anthropogenic aerosols still increase simulated liquid water path
Johannes Mülmenstädt
CORRESPONDING AUTHOR
Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA, USA
Edward Gryspeerdt
Grantham Institute – Climate Change and the Environment, Imperial College London, London, UK
Sudhakar Dipu
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
Johannes Quaas
Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
Andrew S. Ackerman
NASA Goddard Institute for Space Studies, New York, NY, USA
Ann M. Fridlind
NASA Goddard Institute for Space Studies, New York, NY, USA
Florian Tornow
Center for Climate System Research, Columbia University, New York, NY, USA
NASA Goddard Institute for Space Studies, New York, NY, USA
Susanne E. Bauer
NASA Goddard Institute for Space Studies, New York, NY, USA
Andrew Gettelman
Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA, USA
Yi Ming
Schiller Institute for Integrated Science and Society and Department of Earth and Environmental Sciences, Boston College, Boston, MA, USA
Youtong Zheng
Atmospheric and Oceanic Science Program, Princeton University, Princeton, NJ, USA
Department of Earth and Atmospheric Science, University of Houston, Houston, TX, USA
Po-Lun Ma
Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA, USA
Hailong Wang
Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA, USA
Kai Zhang
Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA, USA
Matthew W. Christensen
Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA, USA
Adam C. Varble
Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA, USA
L. Ruby Leung
Atmospheric, Climate, and Earth Sciences Division, Pacific Northwest National Laboratory, Richland, WA, USA
Xiaohong Liu
Department of Atmospheric Sciences, Texas A&M University, College Station, TX, USA
David Neubauer
Institute for Atmospheric and Climate Science, ETH Zürich, Zurich, Switzerland
Daniel G. Partridge
Department of Mathematics and Statistics, University of Exeter, Exeter, UK
Philip Stier
Atmospheric, Oceanic and Planetary Physics, Department of Physics, University of Oxford, Oxford, UK
Toshihiko Takemura
Research Institute for Applied Mechanics, Kyushu University, Fukuoka, Japan
Data sets
US CMS model runs for https://doi.org/10.5194/egusphere-2024-4 J. Mülmenstädt et al. https://doi.org/10.5281/zenodo.10449670
Model code and software
jmuelmen/egusphere-2024-4: egusphere-2024-4 initial ACP submission J. Mülmenstädt https://doi.org/10.5281/zenodo.10449750
Short summary
Human activities release copious amounts of small particles called aerosols into the atmosphere. These particles change how much sunlight clouds reflect to space, an important human perturbation of the climate, whose magnitude is highly uncertain. We found that the latest climate models show a negative correlation but a positive causal relationship between aerosols and cloud water. This means we need to be very careful when we interpret observational studies that can only see correlation.
Human activities release copious amounts of small particles called aerosols into the atmosphere....
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