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The research, led by Dr Arwyn Edwards from Aberystwyth University, focuses on a grainy, soil-like substance found on the surface of Arctic ice known as cryoconite, which is made of dust and industrial soot glued together by photosynthetic bacteria. Working on Greenland’s ice sheet, the team showed that cryoconite darkens the surface of the ice, causing it to melt and make small water-filled holes.
Persistent melt in 2008 lifted the snow cover from a low-lying area of Greenland’s ice sheet, revealing a rough terrain crossed by melt water streams.
Arctic ice reflects about 60% of the sunlight that hits it (known as its albedo level). The cryoconite decreases the albedo of the ice to around 20%, transferring more solar energy to the ice and melting it faster. This bacterial-led albedo reduction is greater than that of dust alone. Working on Svalbard, the group showed that the extreme environmental conditions of the glacier had less of an influence on the communities of microbes present than the effect the microbes themselves had on the melting of the ice. The melt holes that this one species of bacteria form provide an environment for other microbes to flourish, leading to the growth of the cryoconite holes.
“As the biologically productive areas of glaciers and ice sheets expand due to climate change, these microbial processes can influence their melting more and more. In the long term, this contributes to the loss of glacier habitats, and the unique microbial biodiversity living on them.”
Current models are unable to account effectively for the impacts of microbial growth on glacier and ice melting, so learning more about this Arctic ecosystem and the feedback is an important step to understanding future sea level rises.
Benjamin Thompson