Algae Drive Enhanced Darkening of Bare Ice on the Greenland Ice Sheet

Marek Stibal*, Jason E. Box, Karen A. Cameron, Peter L. Langen, Marian L. Yallop, Ruth H. Mottram, Alia L. Khan, Noah P. Molotch, Nathan A M Chrismas, Filippo Calì Quaglia, Daniel Remias, C. J.P.Paul Smeets, Michiel R. van den Broeke, Jonathan C. Ryan, Alun Hubbard, Martyn Tranter, Dirk van As, Andreas P. Ahlstrøm

*Corresponding author for this work

Research output: Contribution to journalArticle (Academic Journal)peer-review

95 Citations (Scopus)
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Surface ablation of the Greenland ice sheet is amplified by surface darkening caused by light-absorbing impurities such as mineral dust, black carbon, and pigmented microbial cells. We present the first quantitative assessment of the microbial contribution to the ice sheet surface darkening, based on field measurements of surface reflectance and concentrations of light-absorbing impurities, including pigmented algae, during the 2014 melt season in the southwestern part of the ice sheet. The impact of algae on bare ice darkening in the study area was greater than that of nonalgal impurities and yielded a net albedo reduction of 0.038 ± 0.0035 for each algal population doubling. We argue that algal growth is a crucial control of bare ice darkening, and incorporating the algal darkening effect will improve mass balance and sea level projections of the Greenland ice sheet and ice masses elsewhere.
Original languageEnglish
Pages (from-to)11463-11471
Number of pages9
JournalGeophysical Research Letters
Issue number22
Early online date18 Nov 2017
Publication statusPublished - 21 Dec 2017


  • Albedo
  • Algae
  • Greenland ice sheet
  • Light-absorbing impurities
  • Meltings


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