Historical black carbon deposition in the Canadian High Arctic: a >250-year long ice-core record from Devon Island
Black carbon aerosol (BC), which is emitted from natural and anthropogenic sources (e.g., wildfires, coal burning), can contribute to magnify climate warming at high latitudes by darkening snow- and ice-covered surfaces, and subsequently lowering their albedo. Therefore, modeling the atmospheric tra...
Published in: | Atmospheric Chemistry and Physics |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Copernicus GmbH
2018
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11937/73688 https://doi.org/10.5194/acp-18-12345-2018 |