https://egusphere.copernicus.org/preprints/2024/egusphere-2024-3063/

*Authors*
Brandon M. Duran, Casey J. Wall, Nicholas J. Lutsko, Takuro Michibata,
Po-Lun Ma, Yi Qin, Margaret L. Duffy, Brian Medeiros, and Matvey Debolskiy

*Citations*: Duran, B. M., Wall, C. J., Lutsko, N. J., Michibata, T., Ma,
P.-L., Qin, Y., Duffy, M. L., Medeiros, B., and Debolskiy, M.: A new method
for diagnosing effective radiative forcing from aerosol-cloud interactions
in climate models, EGUsphere [preprint],
https://doi.org/10.5194/egusphere-2024-3063, 2024.

*Received: 01 Oct 2024 – Discussion started: 02 Oct 2024*

*Abstract*
Aerosol-cloud interactions (ACI) are a leading source of uncertainty in
estimates of the historical effective radiative forcing (ERF). One reason
for this uncertainty is the difficulty of estimating the ERF from
aerosol-cloud interactions (ERFaci) in climate models, which typically
requires multiple calls to the radiation code and cannot disentangle the
contributions from different process to ERFaci. Here, we develop a new,
computationally efficient method for estimating the shortwave (SW) ERFaci
from liquid clouds using histograms of monthly-averaged cloud fraction
partitioned by cloud droplet effective radius (re) and liquid water path
(LWP). Multiplying the histograms with SW cloud radiative kernels gives the
total SW ERFaci from liquid clouds, which can be decomposed into
contributions from the Twomey effect, LWP adjustments, and cloud-fraction
(CF) adjustments. We test the method with data from five CMIP6-era models,
using the Moderate Resolution Imaging Spectroradiometer (MODIS) satellite
instrument simulator to generate the histograms. Our method gives similar
total SW ERFaci estimates to other established methods in regions of
prevalent liquid cloud, and indicates that the Twomey effect, LWP
adjustments, and CF adjustments have contributed −0.34 ± 0.23, −0.22 ±
0.13, and −0.09 ± 0.11 Wm−2, respectively, to the effective radiative
forcing of the climate since 1850 in the ensemble mean (95 % confidence).
These results demonstrate that widespread adoption of a MODIS re– LWP joint
histogram diagnostic would allow the SW ERFaci and its components to be
quickly and accurately diagnosed from climate model outputs, a crucial step
for reducing uncertainty in the historical ERF.

*Source: EGU Sphere*

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