Soot-doped natural snow and its albedo — results from field experiments

Soot has a pronounced effect on the cryosphere and experiments are still needed to reduce the associated uncertainties. This work presents a series of experiments to address this issue, with soot being deposited onto a natural snow surface after which the albedo changes were monitored. The albedo reduction was the most pronounced for the snow with higher soot content, and it was observed immediately following soot deposition. Compared with a previous laboratory study the effects of soot on the snow were not as prominent in outdoor conditions. During snowmelt, about 50% of the originally deposited soot particles were observed to remain at the snow surface. More detailed experiments are however needed to better explain soot's effect on snow and to better quantify this effect. Our albedo versus soot parameterization agreed relatively well with previously published relationships.

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Publication Details

Journal
Työväentutkimus Vuosikirja
Published
2024-12-12
DOI
https://doi.org/10.60910/mzgx-uhjx
Citations
16
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
0.38

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article

Soot-doped natural snow and its albedo — results from field experiments

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Työväentutkimus Vuosikirja
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article

Soot-doped natural snow and its albedo — results from field experiments

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article en
16 citations

Abstract

Soot has a pronounced effect on the cryosphere and experiments are still needed to reduce the associated uncertainties. This work presents a series of experiments to address this issue, with soot being deposited onto a natural snow surface after which the albedo changes were monitored. The albedo reduction was the most pronounced for the snow with higher soot content, and it was observed immediately following soot deposition. Compared with a previous laboratory study the effects of soot on the snow were not as prominent in outdoor conditions. During snowmelt, about 50% of the originally deposited soot particles were observed to remain at the snow surface. More detailed experiments are however needed to better explain soot's effect on snow and to better quantify this effect. Our albedo versus soot parameterization agreed relatively well with previously published relationships.

Työväentutkimus VuosikirjaVol. 21
Finnish Meteorological Institute (FI), Ural Federal University (RU), University of Helsinki (FI), Lund University (SE), Czech University of Life Sciences Prague (CZ), Finnish Geospatial Research Institute (FI), Nanjing University (CN)
Maj ja Tor Nesslingin Säätiö, Koneen Säätiö, Ural Federal University
Climate action
Openalex Percentile: Top 47%
Atmospheric chemistry and aerosols
0.38
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