Articles | Volume 19, issue 24
https://doi.org/10.5194/acp-19-15415-2019
https://doi.org/10.5194/acp-19-15415-2019
Research article
 | 
17 Dec 2019
Research article |  | 17 Dec 2019

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, Edward Gryspeerdt, Marc Salzmann, Po-Lun Ma, Sudhakar Dipu, and Johannes Quaas

Data sets

PRP output used in https://doi.org/10.5194/acp-2018-1304 J. Mülmenstädt, E. Gryspeerdt, M. Salzmann, P.-L. Ma, S. Dipu, and J. Quaas https://doi.org/10.5281/zenodo.3457397

Model code and software

jmuelmen/acp-2018-1304-echam-prp: Zenodo archive release for inclusion in acp-2018-1304 manuscript J. Mülmenstädt, E. Gryspeerdt, M. Salzmann, P.-L. Ma, S. Dipu, and J. Quaas https://doi.org/10.5281/zenodo.3457389

jmuelmen/acp-2018-1304: Zenodo archive release for inclusion in acp-2018-1304 manuscript J. Mülmenstädt, E. Gryspeerdt, M. Salzmann, P.-L. Ma, S. Dipu, and J. Quaas https://doi.org/10.5281/zenodo.3457496

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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.
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