https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1127/

*Authors*
Jianhao Zhang and Graham Feingold

*Received*: 20 Oct 2022
*Discussion started*: 28 Oct 2022 (Preprint)

Abstract
*Marine stratocumuli cool the Earth effectively* due to their *high
reflectance of incoming solar radiation, *and persistent occurrence. The
susceptibility of cloud albedo to droplet number concentration
perturbations depends strongly on large-scale meteorological conditions.
Studies focused on the meteorological dependence of cloud adjustments often
overlook the covariability among meteorological factors and their
geographical and temporal variability. We use 8 years of satellite
observations sorted by day and geographical location to show the global
distribution of *marine low cloud albedo susceptibility. *We find an annual
mean cloud brightening potential for most of the regions, more pronounced
over subtropical coastal regions. Weak cloud darkening potential in the
annual mean is evident over the remote SE Pacific and SE Atlantic. We show
that large-scale meteorological fields from the ERA5 reanalysis data,
including lower-tropospheric stability, free-tropospheric relative
humidity, sea surface temperature, and boundary layer depth, have distinct
covariabilities over each of the eastern subtropical ocean basins where
marine stratocumulus prevail. This leads to markedly different monthly
evolution in albedo susceptibility over each basin. Moreover, we find that
basin-specific regional relationships between key meteorological factors
and albedo susceptibilities are absent in a global analysis. Our results
stress the importance of considering the geographical distinctiveness of
temporal meteorological covariability *when scaling up the local-to-global
response of cloud albedo to aerosol perturbations.*

*Source: EUGsphere*

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