Abstract
Particulate matter (PM) from marine traffic interacts with solar radiation and clouds, ultimately influencing Earth’s radiative balance. Ships operated with conventional fossil fuel oils emit light-absorbing carbonaceous PM that offsets aerosol-driven cooling and can even exert a net positive radiative forcing, i.e. warming effect. Radiative properties of PM are possibly further altered by atmospheric aging processes, the effects of which are not fully understood. We present black carbon (BC) emission factors (EF) and optical properties of fresh and photochemically aged particle emissions from a marine engine, operated using low-sulfur heavy fuel oil (LS-HFO) and marine gas oil (MGO), complying with recent maritime sulfur regulations by the International Maritime Organization (IMO). The fresh particle emissions comprised mostly BC, with average BC EFs of 144 and 43.2 mg/kWh for LS-HFO and MGO, respectively. Light absorption was mostly attributed to BC in particles from both fuels, with absorption Ångström exponent (AAE, 370 to 880 nm) values 0.9–1.0 (interquartile range), and 870 nm single scattering albedo (SSA) values 0.15–0.24 during the full cycles. Fresh LS-HFO emissions exhibited lower SSA values than those of high-sulfur fuels reported in literature, primarily associated with reduced sulfate emissions. Photochemical aging led to an absorption enhancement (Eabs) of 1.2–1.5 and an increase in SSA relative to fresh emissions, although SSA remained below 0.5, and the estimated direct radiative forcing effect stayed positive. Our results show that sulfur-compliant marine fuels can emit highly absorbing particles with an atmospheric warming potential, which is mostly maintained even after photochemical aging.
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Data availability
The main data is available in the online repository DOI:10.5281/zenodo.17344025. Particle mobility size distribution data from the same experiments has been published in Shukla et al. (2025), DOI:10.1039/d5ea00040h. Additional datasets associated with the study are available from the corresponding authors on reasonable request.
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Acknowledgements
This work was funded by the European Union Horizon 2020 project ULTRHAS (project number 955390), Deutsche Forschungsgemeinschaft (DFG, German Research Foundation)—SFB 1477 “Light-Matter Interactions at Interfaces” (project number 441234705), and Research Council of Finland “Black and Brown Carbon in the Atmosphere and the Cryosphere” (BBrCAC) (project number 341597) and “Competitive funding to strengthen university research profiles [PROFI] for the University of Eastern Finland” (project number 352968). Additional funding was provided by Transport Canada. Views and opinions expressed are those of the authors only and do not necessarily reflect those of the European Union. Neither the European Union nor the granting authority can be held responsible for them.
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T.K., A.P., D.S., M.I., A.D., J.S., J.P., A.K., U.E., Z.F. and M.S. carried out the measurements. A.P. processed the data of the HR-ToF-AMS. J.P. processed the data of the SP-MS. T.K. processed the data of other online instruments. T.A.S. conducted the electron microscopy analyses. T.K., V.L. and A.M. performed the OC/EC and UV-vis analyses. T.K. and T.A.S. prepared the graphical figures. H.C., B.B., T.S., T.H., Y.R., J.Ø., R.Z., J.C.C. and O.S. acquired funding and supervised the work. T.K. wrote the main manuscript with inputs from T.A.S., A.P., D.S., M.I., J.P., S.M., A.H., J.C.C. and O.S. T.A.S., A.P., D.S., M.I., J.P., S.M., A.H., H.C., T.S., T.H., Y.R., R.Z., J.C.C. and O.S. reviewed the manuscript.
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Kokkola, T., Sipkens, T.A., Paul, A. et al. Highly light-absorbing particle emissions from low-sulfur marine fuels. npj Clim Atmos Sci (2026). https://doi.org/10.1038/s41612-026-01369-w
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DOI: https://doi.org/10.1038/s41612-026-01369-w


