4.7 Article

Current status and future perspectives of microplastic pollution in typical cryospheric regions

期刊

EARTH-SCIENCE REVIEWS
卷 226, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.earscirev.2022.103924

关键词

Microplastics; Snow; Glaciers; Sea ice; Cryosphere

资金

  1. National Key Research and Development Program of China [2020YFA0608503]
  2. National Natural Science Foundation of China [42071082]
  3. State Key Laboratory of Cryospheric Science [SKLCS-ZZ-2021]
  4. CAS Light of West China Program
  5. Leverhulme Trust [ECF-2019-309]
  6. Carnegie Trust
  7. University of Strathclyde (UK)
  8. second Tibetan Plateau Scientific Expedition and Research Program [2019QZKK0605]

向作者/读者索取更多资源

The cryosphere refers to the frozen areas on Earth, including snow and ice, which are being increasingly polluted by microplastics. This review highlights the distribution, transport pathways, and differences in microplastics found in snow and ice across cryospheric regions. It emphasizes the urgent need for improved standard procedures in sampling, pretreatment, and identification of microplastics. The study suggests that sea ice and atmospheric transport play important roles in the temporal storage and release of microplastics, while non-polar cryospheric regions may serve as important receptors of microplastics from mid-latitude emissions, posing potential climate risks.
The cryosphere is the term used to describe the frozen areas of the Earth, including all forms of snow and ice, which are primarily influenced by anthropogenic pollutants through atmospheric transport. In this review, we described the current status of newly emergent pollutant-microplastics-in the snow and ice of typical cryospheric regions (e.g., Arctic, Antarctic, Alps, Tibetan Plateau, and Andes), discussed their transport pathways, and provided perspectives for future research. A brief summary of snow and ice sampling, pretreatment, and the identification of microplastics in cryospheric regions suggested that standard procedures were inadequate and urgently required improvement. Microplastics were widely distributed in snow and ice across the typical cryospheric regions, indicating the ubiquitous distribution of microplastics in such environments. However, the abundance, size distribution, shape, and polymer composition of the microplastics in snow and ice showed significant differences. Sea ice was especially important for the temporal storage, transport, and release of microplastics in the Arctic and Antarctic. Microplastics in land snow cover and mountain glaciers emphasized the importance of atmospheric transport in the transferal of microplastics to cryospheric regions. In particular, the non-polar cryospheric regions (e.g., Tibetan Plateau, Andes, or Alps) were highlighted as important receptors of mid-latitude emissions of microplastics, which might indicate a future climatic risk considering the ability of microplastics to absorb radiation and accelerate the melting of snow. Microplastics retrieved from mountain glacier ice cores may also provide new insights into the historical variations of anthropogenic pollutants. The potential impact of microplastics in snow and ice on the carbon cycle and the climatic risk needs to be further addressed in the future.

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