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Dark microplastics trigger changes on snow metamorphism that depends on the snow initial density
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Field experiments in the Spanish Pyrenees tested how dark microplastic particles affect snow, finding that effects depended heavily on the snow's age and density. On fresh, light snow, microplastics caused changes in snow crystal structure but minimal extra melting; on older, denser snow, heavy microplastic accumulation increased melt rates by 17% compared to uncontaminated snow. This is the first field evidence that microplastics can accelerate snowmelt, with implications for water supply timing and glacier loss in mountain regions.
Cryospheric regions are no exception to microplastic ubiquity. Still, microplastic's capacity to decrease snow albedo or advance snow melting, as light-absorbing impurities, remains unexplored. This study assesses the effect of dark microplastics on snow properties under realistic conditions. Six experiments were conducted at the Central Pyrenees (Spain), exposing surface snow to different concentrations of dark micropellets for 4 h. Results were variable and dependent on snow initial conditions. In the experiments performed on recent, light snow (<250 kg m), increasing concentrations of microplastics yielded moderate decreases in albedo and high changes in snow specific surface area, reducing it by 11.4 m kg as compared to blank samples, while snowmelt changes were <1%. On the contrary, in the experiments conducted on aged snow of high density (>450 kg m), high microplastic accumulation increased snowmelt 17% more than in the blanks. Further field studies are needed for a better understanding of the effect of microplastics on the global cryosphere.
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On the role of Microplastics as Light Absorbing Particles in seasonal snowpacks: First evidence from the Central Pyrenees
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Researchers conducted six in situ lysimeter experiments in the Spanish Central Pyrenees during the 2023-2024 snow season, providing the first experimental evidence that microplastic particles act as light-absorbing impurities capable of affecting snow albedo and metamorphism in seasonal mountain snowpacks.
Microplastics’ Hidden Contribution to Snow Melting
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Microplastic particles present in snow can reduce its reflectivity (albedo) by absorbing sunlight, contributing to faster snow melting and potentially affecting Earth's radiative balance. This subtle effect means microplastic pollution in snow and ice may be compounding the impacts of black carbon on polar and mountain snow melt.
Microplastic particles in dust-on-snow, Upper Colorado River Basin, Colorado Rocky Mountains, 2013–16
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Researchers found microplastic particles in dust-on-snow samples from the Upper Colorado River Basin collected between 2013 and 2016, providing early evidence that atmospheric deposition delivers microplastics to mountain snowpack. These particles join mineral dust in reducing snow reflectivity, potentially accelerating snowmelt and affecting regional water supplies.
Analysis of small microparticles from snow in Park City, Utah (USA): How much of it is plastic?
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Fresh snow samples from ski areas in Park City, Utah contained 1,000–4,000 small microparticles per 50 mL, with a mix of synthetic polymers (nylon, polyester, PVC, polyethylene) and natural fibers, and—surprisingly—higher concentrations at a more remote, higher-altitude site than at lower-elevation resort areas. The results suggest that atmospheric deposition is carrying microplastics to mountain snowpack regardless of local human activity, and that concentrations at the high-altitude site have increased over the study period. Snow is an important reservoir and transport medium for microplastics, and mountain snowmelt may be delivering these particles into downstream watersheds.
Microplastics have light-absorbing ability to enhance cryospheric melting
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Researchers found that microplastics have light-absorbing properties that may reduce snow and ice surface albedo in polar and glacial regions, suggesting airborne microplastic deposition could accelerate cryospheric melting and represent an underappreciated feedback in global warming.
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