Report: Unaccounted for Arctic microbes appear to be speeding up glacier melting

A process not accounted for in current climate change models. So there should be even more warming occurring than isn’t?

The media release is below.

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Unaccounted for Arctic microbes appear to be speeding up glacier melting
SOCIETY FOR GENERAL MICROBIOLOGY

Today, at the Microbiology Society’s Annual Conference in Liverpool, scientists will reveal how Arctic microbes are increasing the rate at which glaciers melt, in a process not accounted for in current climate change models.

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. The bacterially-made granules self-regulate the depth and shape of these holes to maximise their exposure to sunlight, which in turn further melts the glacier’s surface ice. In summer, cryoconite holes pockmark the surface of the biologically productive region of the Greenland ice sheet, an area ten times the size of Wales (200,000 square kilometres), which is expanding as the climate warms.

Working on an icecap in Svalbard, in the far north of Norway, the team showed that this process is driven by a single species of photosynthetic bacteria, from the genus Phormidesmis.

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.

Dr Edwards said: “If we recognise ice surfaces as a living landscape we can see that the microbes themselves are able to change the glacial surface. It’s only recently that we’ve begun to understand that these cryoconite holes are dynamic, changing in size and shape. Microbes are capable of ecosystem engineering and respond to changes in their environment all the time.

“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.

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4 thoughts on “Report: Unaccounted for Arctic microbes appear to be speeding up glacier melting”

  1. ” a process not accounted for in current climate change models”
    These seem to be cropping up almost regularly.

  2. “Microbes are capable of ecosystem engineering and respond to changes in their environment all the time.”
    Selfish life forms have been altering their environment with their accumulating wastes for 3.5 billion years, when they started doing photosynthesis.

  3. Wait what!! It’s BS I tell you! Surely, it must really just be “microbial human life-forms” making all the …

  4. http://notrickszone.com/2016/03/24/new-vast-body-of-literature-shows-rates-of-glacier-retreat-sea-level-change-now-significantly-lower/#sthash.0pi7mPhT.dpbs

    “According to recently published scientific papers, the current sea level highstand, as well as the rate of glacier retreat and sea level change, are now significantly lower than they have been for much of the last 10,000 years — back when CO2 concentrations were stable and considerably lower (at about 265 ppm). “

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