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...
| Main Authors: | , , , , , , |
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| Format: | Journal Article |
| Published: |
Copernicus GmbH
2018
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| Online Access: | http://hdl.handle.net/20.500.11937/73688 |