Distinct regional meteorological influences on low cloud albedo susceptibility over global marine stratocumulus regions

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 and reanalysis data sorted by day and geographical location to show that large-scale meteorological factors, including lower-tropospheric stability, freetropospheric 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. 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.

The Role of Mesoscale Cloud Morphology in the Shortwave Cloud Feedback

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Hidden Large Aerosol‐Driven Cloud Cover Effect Over High‐Latitude Ocean

“…A mixed response of liquid‐phase cloud water prompted by unpolluted and polluted clouds was indicated (Toll et al., 2019), resulting in a weak decrease in water amount in the polluted background and a slight increase in a clean background. Since the aerosol‐induced effects are significant in a clean background as indicated by smaller N d , it is necessary to evaluate the overall aerosol effects thoroughly as a function of background N d (Hu et al., 2021; J. Zhang & Feingold, 2022).…”