Showing posts with label dark snow. Show all posts
Showing posts with label dark snow. Show all posts

Monday, 10 November 2014

Dark Snow

Just one of 38 positive feedbacks

Greenland Ice Is Turning Black, and That’s Not the Bad News


7 November, 2014


It isn’t just happening in Greenland. It’s happening in the Himalayas, in western North America, in the Arctic circle. For the past few decades, glaciers and ice sheets in these locations are turning black, darkening from soot and other pollutants. Sure, it’s an aesthetic problem, but black ice leads to a much larger and more dangerous problem: Sea level rise.


In the Tibetan Himalayas, dung and wood are used to fuel cooking stoves. Over time, the soot produced by these fires has drifted on the wind and settled on the surrounding glaciers – glaciers that feed the Yangtze, Yellow, Mekong and Ganges rivers and sustain two billion people. A 2009 study from the Proceedings of the National Academy of Sciences suggests that this soot, coupled with global warming trends, is playing a key role in melting the Himalayan glaciers.


This is because the soot decreases snow’s “albedo,” its ability to reflect solar energy back into space. White snow, ice and clouds can reflect a portion of the sun’s rays and remain cool, even when they cover large areas. Darker areas, however, even small ones, absorb the sun’s heat much more easily. Thus, as snow darkens, it melts much more easily.


The effect of soot on Himalayan glaciers is the same observed on Greenland’s ice sheets. Utilizing remote sensing data, a report published in Nature Geoscience earlier this year “indicates that the springtime darkening [of the Greenland ice sheet] since 2009 stems from a widespread increase in the amount of light-absorbing impurities in snow, as well as in the atmosphere.”


The soot that’s blackening the ice comes from multiple sources: pollen and dust, industrial and automotive exhaust, and forest fires. In early October, Jason Box from the Geological Survey of Denmark and Greenland reported that there had been more forest fires in the northern hemisphere this year than any year in the last decade.


America, for example, is experiencing drier conditions and longer fire seasons, which has resulted in bigger, costlier wildfires along its west coast. Fires have been so severe that the state exhausted its larger-than-average $209 million fire-fighting budget in the first three months of the fiscal year.


Recently, Box used drones to survey Greenland’s darkening ice. The damage can be glimpsed in the video below.




The Arctic is warming up twice as fast as the Subarctic, and we think it may be due to the dark ice that absorbs the sun’s rays rather than reflecting them as white ice would,” Box told ScienceNordic. “Therefore, it is important that we get a better understanding of the significance of the dark ice.”


As the temperature rises, microbes are finding it easier to survive in the Arctic. Algae is beginning to thrive in Greenland, which further minimizes the area’s albedo and accelerates the melting process.The microbes are currently getting more space to live and grow,” says Box’s colleague, Marek Stibal. “Moreover, they are not dependent on being brought by the wind, and it makes their contribution even more significant.”


Black ice and snow is very likely a contributing factor to the “unprecedented rate” of volume loss in the Greenland ice sheet observed by the European Space Agency’s CryoSatellite. As global ice sheets continue to blacken, they will melt even faster, potentially leading to more advanced sea level rise by the end of this century than previously predicted.



Thursday, 30 October 2014

Dark Snow

About the August, 2014 dark Greenland photos
Jason Box


29 October, 2014


Photos and video I took during an August 2014 south Greenland maintenance tour of promice.org climate stations and an extreme ice survey time lapse camera went viral, featuring a surprisingly (to me and others) dark surface of Greenland ice.
Photo by Jason Box
Photo by Jason Box
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What we know, the southern Greenland ice sheet hit record low reflectivity in the period of satellite observations since 2000 due to a ~2 month drought affecting south Greenland….

nland…
2014_August_record_map
map with colors indicating when record low albedo was observed. The photos are from the blue patch near the southern tip of Greenland.
Snowfall summer 2014  for south Greenland would have kept the melt rates down by brightening up the surface. Summer 2014, at the PROMICE.org QAS_A site, we recorded ice loss from the surface at a place we thought was above equilibrium line altitude, where the surface would lose no ice in an ‘average climate’. The higher than normal melt rates allowed the impurities to concentrate near the surface in a process documented for snow surfaces by Doherty et al. (2013).

To avoid misinterpretation, black carbon is only part of the darkness, the rest is dust and microbes (See Dumont et al. 2014 and Benning et al. 2014). The photos are from the lowest part of the ice sheet’s elevation. The upper elevations do not get nearly this dark. This satellite image illustrates for west Greenland how dark the surface gets, down to 30% reflectivity.

Work Cited
  • Benning, L.G. A.M. Anesio, S. Lutz & M. Tranter, Biological impact on Greenland’s albedo, Nature Geoscience 7, 691 (2014) doi:10.1038/ngeo2260
  • Doherty, S. J., T. C. Grenfell, S. Forsstro¨ m, D. L. Hegg, R. E. Brandt, and S. G. Warren (2013), Observed vertical redistribution of black carbon and other insoluble light-absorbing particles in melting snow, J. Geophys. Res. Atmos., 118, 5553–5569, doi:10.1002/jgrd.50235.
  • Dumont, M., E. Brun, G. Picard, M. Michou, Q. Libois, J-R. Petit, M. Geyer, S. Morin and B. Josse, Contribution of light-absorbing impurities in snow to Greenland’s darkening since 2009, Nature Geoscience, 8 June, 2014, DOI: 10.1038/NGEO2180



Photo by Jason Box
Photos by Jason Box

For the website Dark Snow GO HERE





This lecture is from January, 2013