Algae drive enhanced darkening of bare ice on the Greenland ice sheet

Marek Stibal, Jason Box, Karen 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. Paul Smeets, Michiel R. van den Broeke, Jonathan Ryan, Alun Hubbard, Martyn Tranter, Dirk Van As, Andreas P. Ahlstrøm

Allbwn ymchwil: Cyfraniad at gyfnodolynErthygladolygiad gan gymheiriaid

97 Dyfyniadau(SciVal)
419 Wedi eu Llwytho i Lawr (Pure)

Crynodeb

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 non-algal 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
Iaith wreiddiolSaesneg
Tudalennau (o-i)11463-11471
Nifer y tudalennau9
CyfnodolynGeophysical Research Letters
Cyfrol44
Rhif cyhoeddi22
Dyddiad ar-lein cynnar18 Tach 2017
Dynodwyr Gwrthrych Digidol (DOIs)
StatwsCyhoeddwyd - 28 Tach 2017

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