Car microplastic pollution rides the wind... all the way to the Arctic

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Jan Kopřiva on Unsplash
Jan Kopřiva on Unsplash

Tyre and brake pad wear accounts for about a third of all microplastic pollution, and Norwegian research finds that literal tonnes of it are carried through the atmosphere. The authors found that 52,000 tonnes of road microplastics are blown into the world's oceans every year, and a further 20,000 tonnes end up on remote snow and ice. They suggest the light-absorbing properties of car microplastics may also speed up Arctic warming and melting.

Media release

From: Springer Nature

The atmospheric transportation around the world of microplastics produced by road traffic is modelled in a paper in Nature Communications. The study finds that microplastic particles are transported to remote regions, including the Arctic. Estimates suggest that the total amount of these particles which end up in the oceans as a result of airborne delivery is of a similar size to that deposited by rivers.

As the production rate of new plastic products continues to increase, ever greater quantities evade waste collection and recycling. However, the ecological and environmental consequences of rising plastic pollution, and the routes they take to get there, are poorly understood.

Nikolaos Evangeliou and colleagues combine a global quantification of road microplastics (produced from tyre wear and brake wear) with simulations of atmospheric transport pathways to determine the trajectory of these pollutants. Road microplastic emissions currently constitute 30% of microplastic pollution, the majority of which comes from densely populated regions like the eastern US, Northern Europe and the heavily urbanized areas of Southeast Asia. The authors found that larger particles were deposited close to the source of production. Conversely, microplastics that are 2.5 micrometers and smaller in size were transported further afield. They estimate that 52,000 tonnes per year of the small size microplastics end up in the world’s oceans. However, around 14% (20,000 tonnes per year) ends up on remote snow- and ice-covered surfaces. The authors note that this is concerning for sensitive regions, such as the Arctic, because the dark particles decrease surface albedo (the amount of sunlight reflected from the Earth’s surface) and could hasten melting.

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Research Springer Nature, Web page
Journal/
conference:
Nature Communications
Research:Paper
Organisation/s: Norwegian Institute for Air Research, Norway
Funder: This work was supported by COMBAT (Quantification of Global Ammonia Sources constrained by a Bayesian Inversion Technique) funded by ROMFORSK—Program for romforskning of the Research Council of Norway (Project ID: 275407), website: https:// www.forskningsradet.no/prosjektbanken/#/project/NFR/275407.
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