Unprecedented radioactive pollution in Spitsbergen's air-first data of the 21st century

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Abstract

This study investigated the Arctic troposphere, providing a comprehensive experimental database on nuclear aerosols that has significantly improved since 1999. The activity concentrations of 238Pu, 239+240Pu, and 241Am were measured in surface air at Hornsund, Spitsbergen, from 2007–2021. A multivariate approach, incorporating meteorological data, gamma-emitter records, and isotopic ratios, was employed to explain the dynamics of change and the provenance of transuranium elements. Levels of 238Pu and 239+240Pu were found comparable to those documented over the past decades at various locations. The highest activity concentrations were 6.61 nBqm-3 for 238Pu and 15.5 nBqm-3 for 239+240Pu, observed in 2015. Although coinciding with the resuspension and atmospheric transport of radionuclides due to the 2015 wildfires near the Chernobyl zone, a direct contribution to Hornsund remains uncertain. Further data exploration revealed a correlation between 239+240Pu and seasonal processes, including local dust redistribution and horizontal tropospheric transport of haze layers from distant areas. While similar mechanisms likely regulated a portion of 238Pu, its random enrichment relative to known nuclear events was frequently detected. As a general trend, 241Am exhibited notably high activity concentrations, reaching up to 354 nBqm-3 in 2019. Episodic signals of 237Np were identified in 2013, 2014, and 2018. All occurrences of 241Am, 237Np, and outliers of 238Pu were not linked to natural processes; hence, the possibility of recent radioactive emissions should be considered. Trajectory simulations conducted for 2019 indicated prominent transport pathways to Hornsund from northern Eurasia.

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Cwanek, A., Burakowska, A., Nalichowska, E., Długosz-Lisiecka, M., Kubicki, M., Wawrzyniak, T., … Lubera, G. (2026). Unprecedented radioactive pollution in Spitsbergen’s air-first data of the 21st century. Atmospheric Chemistry and Physics, 26(8), 5839–5860. https://doi.org/10.5194/acp-26-5839-2026

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