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

<p>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...

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Main Authors: J. Zhang, G. Feingold
Format: Article
Language:English
Published: Copernicus Publications 2023-01-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/23/1073/2023/acp-23-1073-2023.pdf
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author J. Zhang
J. Zhang
G. Feingold
author_facet J. Zhang
J. Zhang
G. Feingold
author_sort J. Zhang
collection DOAJ
description <p>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 overall cloud brightening potential for most marine warm clouds, which is more pronounced over subtropical coastal regions. A 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 stratocumuli prevail. This leads to a markedly different annual cycle 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.</p>
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spelling doaj.art-b3a104f7976e4a2bad283558577ea0b72023-01-20T12:29:08ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242023-01-01231073109010.5194/acp-23-1073-2023Distinct regional meteorological influences on low-cloud albedo susceptibility over global marine stratocumulus regionsJ. Zhang0J. Zhang1G. Feingold2Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, CO, USAChemical Sciences Laboratory, National Oceanic and Atmospheric Administration (NOAA), Boulder, CO, USAChemical Sciences Laboratory, National Oceanic and Atmospheric Administration (NOAA), Boulder, CO, USA<p>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 overall cloud brightening potential for most marine warm clouds, which is more pronounced over subtropical coastal regions. A 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 stratocumuli prevail. This leads to a markedly different annual cycle 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.</p>https://acp.copernicus.org/articles/23/1073/2023/acp-23-1073-2023.pdf
spellingShingle J. Zhang
J. Zhang
G. Feingold
Distinct regional meteorological influences on low-cloud albedo susceptibility over global marine stratocumulus regions
Atmospheric Chemistry and Physics
title Distinct regional meteorological influences on low-cloud albedo susceptibility over global marine stratocumulus regions
title_full Distinct regional meteorological influences on low-cloud albedo susceptibility over global marine stratocumulus regions
title_fullStr Distinct regional meteorological influences on low-cloud albedo susceptibility over global marine stratocumulus regions
title_full_unstemmed Distinct regional meteorological influences on low-cloud albedo susceptibility over global marine stratocumulus regions
title_short Distinct regional meteorological influences on low-cloud albedo susceptibility over global marine stratocumulus regions
title_sort distinct regional meteorological influences on low cloud albedo susceptibility over global marine stratocumulus regions
url https://acp.copernicus.org/articles/23/1073/2023/acp-23-1073-2023.pdf
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AT jzhang distinctregionalmeteorologicalinfluencesonlowcloudalbedosusceptibilityoverglobalmarinestratocumulusregions
AT gfeingold distinctregionalmeteorologicalinfluencesonlowcloudalbedosusceptibilityoverglobalmarinestratocumulusregions