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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 5
The Cryosphere, 9, 1845–1856, 2015
https://doi.org/10.5194/tc-9-1845-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Interactions between climate change and the Cryosphere: SVALI,...

The Cryosphere, 9, 1845–1856, 2015
https://doi.org/10.5194/tc-9-1845-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 22 Sep 2015

Research article | 22 Sep 2015

Ice sheet mass loss caused by dust and black carbon accumulation

T. Goelles et al.

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Revised manuscript not accepted
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Cited articles

Ahlkrona, J., Kirchner, N., and Lötstedt, P.: A numerical study of scaling relations for non-newtonian thin-film flows with applications in ice sheet modelling, Q. J. Mech. Appl. Math., 66, 417–435, https://doi.org/10.1093/qjmam/hbt009, 2013.
Bamber, J. L., Griggs, J. A., Hurkmans, R. T. W. L., Dowdeswell, J. A., Gogineni, S. P., Howat, I., Mouginot, J., Paden, J., Palmer, S., Rignot, E., and Steinhage, D.: A new bed elevation dataset for Greenland, The Cryosphere, 7, 499–510, https://doi.org/10.5194/tc-7-499-2013, 2013.
Bauer, S. E., Bausch, A., Nazarenko, L., Tsigaridis, K., Xu, B., Edwards, R., Bisiaux, M., and McConnell, J.: Historical and future black carbon deposition on the three ice caps: ice core measurements and model simulations from 1850 to 2100, J. Geophys. Res.-Atmos., 118, 7948–7961, https://doi.org/10.1002/jgrd.50612, 2013.
Bigler, M.: New aerosol measurements from the Greenland NEEM ice core, in: EGU General Assembly Conference Abstracts, 22–27 April 2012, Vienna, Austria, 5780 pp., 2012.
Biscaye, P. E., Grousset, F. E., Revel, M., van der Gaast, S., Zielinski, G. A., Vaars, A., and Kukla, G.: Asian provenance of glacial dust (stage 2) in the Greenland Ice Sheet Project 2 Ice Core, Summit, Greenland, J. Geophys. Res.-Oceans, 102, 26765–26781, https://doi.org/10.1029/97JC01249, 1997.
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Short summary
Soot (black carbon) and dust particles darken the surface of ice sheets and glaciers as they accumulate. This causes more ice to melt, which releases more particles from within the ice. This positive feedback mechanism is studied with a new two-dimensional model, mimicking the conditions of Greenland, under different climate warming scenarios. In the warmest scenario, the additional ice sheet mass loss until the year 3000 is up to 7%.
Soot (black carbon) and dust particles darken the surface of ice sheets and glaciers as they...
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