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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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We quantify aerosol–cloud radiative interactions in a regime of deep open-cell stratocumuli (boundary layer depth 1.5 km), a regime which remains largely unexplored within this context and yet is more dominant than cases of shallow stratocumuli previously studied. We simulate substantial increases in albedo in a regime where ship tracks are not found and argue that such changes may escape detection and attribution through remote sensing due to the large natural variability in the system.
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ACP | Articles | Volume 18, issue 23
Atmos. Chem. Phys., 18, 17475–17488, 2018
https://doi.org/10.5194/acp-18-17475-2018
Atmos. Chem. Phys., 18, 17475–17488, 2018
https://doi.org/10.5194/acp-18-17475-2018

Research article 11 Dec 2018

Research article | 11 Dec 2018

The efficacy of aerosol–cloud radiative perturbations from near-surface emissions in deep open-cell stratocumuli

Anna Possner et al.

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Latest update: 22 Jan 2021
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Short summary
We quantify aerosol–cloud radiative interactions in a regime of deep open-cell stratocumuli (boundary layer depth 1.5 km), a regime which remains largely unexplored within this context and yet is more dominant than cases of shallow stratocumuli previously studied. We simulate substantial increases in albedo in a regime where ship tracks are not found and argue that such changes may escape detection and attribution through remote sensing due to the large natural variability in the system.
Citation
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Final-revised paper
Preprint