Impact on cloud properties of reduced-sulphur shipping fuel in the Eastern North Atlantic

Abstract. The global reduction in shipping fuel sulphur that culminated in 2020 with an ∼ 80 % reduction has created a large-scale natural experiment on the role of aerosol-cloud interaction (ACI) in the climate system. We compare observations from the Atmospheric Radiation Measurement program's Eastern North Atlantic site (ARM-ENA; 39.1° N, 28.0° W) during two June to September periods: 2016–2018 (pre-2020) and 2021–2023 (post-2020). We find a significant (∼ 15 %) decrease in cloud condensation nuclei concentrations post-2020, which resulted in a decrease in cloud droplet number (Nd) and an increase in effective radius (re) of marine boundary layer clouds. However, cloud liquid water path (LWP) increased post-2020. The increase in LWP offset the increase in re, resulting in insignificant changes to optical depth. MODIS and CERES data in the vicinity of ENA during these periods produce similar results also with negligible change in albedo and optical depth. Regional cloud occurrence declined in line with changes in the large-scale meteorology. Our results highlight the complex interplay of factors that modulate cloud feedbacks in the Eastern North Atlantic.

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Journal
Atmospheric chemistry and physics
Published
2026-01-22
DOI
https://doi.org/10.5194/acp-26-1041-2026
Primary Topic
Atmospheric chemistry and aerosols
Type
article
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Impact on cloud properties of reduced-sulphur shipping fuel in the Eastern North Atlantic

Peter M. Gombert, Sally Benson, Tiffany Smallwood, Gerald G. Mace
Atmospheric chemistry and physics
Atmospheric chemistry and aerosols
article

Impact on cloud properties of reduced-sulphur shipping fuel in the Eastern North Atlantic

Peter M. Gombert, Sally Benson, Tiffany Smallwood, Gerald G. Mace
article en

Abstract

Abstract. The global reduction in shipping fuel sulphur that culminated in 2020 with an ∼ 80 % reduction has created a large-scale natural experiment on the role of aerosol-cloud interaction (ACI) in the climate system. We compare observations from the Atmospheric Radiation Measurement program's Eastern North Atlantic site (ARM-ENA; 39.1° N, 28.0° W) during two June to September periods: 2016–2018 (pre-2020) and 2021–2023 (post-2020). We find a significant (∼ 15 %) decrease in cloud condensation nuclei concentrations post-2020, which resulted in a decrease in cloud droplet number (Nd) and an increase in effective radius (re) of marine boundary layer clouds. However, cloud liquid water path (LWP) increased post-2020. The increase in LWP offset the increase in re, resulting in insignificant changes to optical depth. MODIS and CERES data in the vicinity of ENA during these periods produce similar results also with negligible change in albedo and optical depth. Regional cloud occurrence declined in line with changes in the large-scale meteorology. Our results highlight the complex interplay of factors that modulate cloud feedbacks in the Eastern North Atlantic.

Atmospheric chemistry and physicsVol. 26(2)
University of Utah (US)
Climate action, Life below water
Openalex Percentile: Top 85%
Atmospheric chemistry and aerosols
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Impact on cloud properties of reduced-sulphur shipping fuel in the Eastern North Atlantic — Peter M. Gombert, Sally Benson, et al. · Atmospheric chemistry and physics (2026) | TGRS Research Map | TGRS