Articles | Volume 19, issue 24
https://doi.org/10.5194/acp-19-15415-2019
© Author(s) 2019. 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-19-15415-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Separating radiative forcing by aerosol–cloud interactions and rapid cloud adjustments in the ECHAM–HAMMOZ aerosol–climate model using the method of partial radiative perturbations
Johannes Mülmenstädt
CORRESPONDING AUTHOR
Institute of Meteorology, Universität Leipzig, Leipzig, Germany
now at: Pacific Northwest National Laboratory, Richland, Washington, USA
Edward Gryspeerdt
Space and Atmospheric Physics Group, Imperial College London, London, UK
Marc Salzmann
Institute of Meteorology, Universität Leipzig, Leipzig, Germany
Po-Lun Ma
Pacific Northwest National Laboratory, Richland, Washington, USA
Sudhakar Dipu
Institute of Meteorology, Universität Leipzig, Leipzig, Germany
Johannes Quaas
Institute of Meteorology, Universität Leipzig, Leipzig, Germany
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- Separating radiative forcing by aerosol–cloud interactions and rapid cloud adjustments in the ECHAM–HAMMOZ aerosol–climate model using the method of partial radiative perturbations J. Mülmenstädt et al. 10.5194/acp-19-15415-2019
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16 citations as recorded by crossref.
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- Coupling aerosols to (cirrus) clouds in the global EMAC-MADE3 aerosol–climate model M. Righi et al. 10.5194/gmd-13-1635-2020
- Snow-induced buffering in aerosol–cloud interactions T. Michibata et al. 10.5194/acp-20-13771-2020
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- The decomposition of cloud–aerosol forcing in the UK Earth System Model (UKESM1) D. Grosvenor & K. Carslaw 10.5194/acp-20-15681-2020
- An underestimated negative cloud feedback from cloud lifetime changes J. Mülmenstädt et al. 10.1038/s41558-021-01038-1
- Comparing the Radiative Forcings of the Anthropogenic Aerosol Emissions From Chile and Mexico T. Miinalainen et al. 10.1029/2020JD033364
- Effective radiative forcing and adjustments in CMIP6 models C. Smith et al. 10.5194/acp-20-9591-2020
- Evaluation of liquid cloud albedo susceptibility in E3SM using coupled eastern North Atlantic surface and satellite retrievals A. Varble et al. 10.5194/acp-23-13523-2023
- Increasing aerosol direct effect despite declining global emissions in MPI-ESM1.2 A. Hermant et al. 10.5194/acp-24-10707-2024
- Reducing the aerosol forcing uncertainty using observational constraints on warm rain processes J. Mülmenstädt et al. 10.1126/sciadv.aaz6433
- The Impact of Resolving Subkilometer Processes on Aerosol‐Cloud Interactions of Low‐Level Clouds in Global Model Simulations C. Terai et al. 10.1029/2020MS002274
- Cloud, Aerosol, and Radiative Properties Over the Western North Atlantic Ocean R. Braun et al. 10.1029/2020JD034113
- Sensitivity of cloud microphysics to aerosol is highly associated with cloud water content: Implications for indirect radiative forcing Y. Wang et al. 10.1016/j.atmosres.2024.107552
2 citations as recorded by crossref.
- Separating radiative forcing by aerosol–cloud interactions and rapid cloud adjustments in the ECHAM–HAMMOZ aerosol–climate model using the method of partial radiative perturbations J. Mülmenstädt et al. 10.5194/acp-19-15415-2019
- Surprising similarities in model and observational aerosol radiative forcing estimates E. Gryspeerdt et al. 10.5194/acp-20-613-2020
Latest update: 14 Dec 2024
Short summary
The effect of aerosol–cloud interactions (ACIs) on Earth's energy budget continues to be highly uncertain. We decompose the effective radiative forcing by ACIs (ERFaci) into the instantaneous forcing due to anthropogenic increases in the number of cloud droplets and fast responses of cloud properties to the droplet number perturbation in the ECHAM–HAMMOZ aerosol–climate model. This decomposition maps onto the IPCC's Fifth Assessment Report analysis of ERFaci more directly than previous work.
The effect of aerosol–cloud interactions (ACIs) on Earth's energy budget continues to be highly...
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