Brief communication: Light-absorbing impurities can reduce the density of melting snow

Climatic effects of black carbon (BC) deposition on snow have been proposed to result from reduced snow albedo and increased melt due to light-absorbing particles. In this study, we hypothesize that BC may decrease the liquid-water retention capacity of melting snow, and present our first data, wher...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Meinander, O., Kontu, A., Virkkula, A., Arola, A., Backman, L., Dagsson-Waldhauserová, P., Järvinen, O., Manninen, T., Svensson, J., de Leeuw, G., Leppäranta, M.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2014
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article
Verlagsveröffentlichung
The Cryosphere
Online Access:https://doi.org/10.5194/tc-8-991-2014
https://noa.gwlb.de/receive/cop_mods_00019926
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00019881/tc-8-991-2014.pdf
https://tc.copernicus.org/articles/8/991/2014/tc-8-991-2014.pdf
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Summary:Climatic effects of black carbon (BC) deposition on snow have been proposed to result from reduced snow albedo and increased melt due to light-absorbing particles. In this study, we hypothesize that BC may decrease the liquid-water retention capacity of melting snow, and present our first data, where both the snow density and elemental carbon content were measured. In our experiments, artificially added light-absorbing impurities decreased the density of seasonally melting natural snow. No relationship was found in case of natural non-melting snow. We also suggest three possible processes that might lead to lower snow density.

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