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Assessment of the impact of glacial algae and abiotic impurities on the melting of the Greenland ice sheet

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Global warming is leading to considerable loss of ice mass from glaciers worldwide and the melting of the Greenland Ice Sheet (GrIS) is a particular threat to coastal communities. The most current measurements indicate that the GrIS alone is responsible for a significant part of sea level rise. Most ice loss occurs along the southern and western margins of the GrIS, which coincides with a large dark area on the surface of the ice. The darker the ice gets, the more radiation is absorbed, generating heat and more melt. Initially, researchers speculated that high concentrations of old dust melting out of the ice and increased atmospheric deposition of black or brown carbon were the main cause of the darkening of the ice. However, it is now well recognized that local biological factors have a much relevant impact. Microscopic plants, specialized and able to thrive on ice surfaces (glacier ice algae), are the dominant darkening (and thus, melt enhancing) component of the western Greenland ice sheet. Based on the current knowledge of the biology of glacier ice algae, we suggest ice algal blooms (and thus ice darkening) are likely to increase as a consequence of climate warming and should be taken into account in the estimations of ice mass loss in the future.
Original languageEnglish
PublisherAarhus Universitet, DCE - Nationalt Center for Miljø og Energi
Number of pages24
ISBN (Print)978-87-7156-657-4
Publication statusPublished - Jan 2022
SeriesScientific Report from DCE - Danish Centre for Environment and Energy

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