An 800-year high-resolution black carbon ice core record from Lomonosovfonna, Svalbard, Atmos
Produced by the incomplete combustion of fossil fuel and biomass, black carbon (BC) contributes to Arctic warming by reducing snow albedo and thus triggering a snow-albedo feedback leading to increased snowmelt. Therefore, it is of high importance to assess past BC emissions to better understand and...
Main Authors: | , , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
2018
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Subjects: | |
Online Access: | https://hdl.handle.net/10669/85130 https://acp.copernicus.org/articles/18/12777/2018/ https://doi.org/10.5194/acp-2018-244 |