Journal article
Global and regional climate changes due to black carbon
Nature geoscience, Vol.1(4), pp.221-227
2008
DOI: 10.1038/ngeo156
Abstract
Black carbon in soot is the dominant absorber of visible solar radiation in the atmosphere. Anthropogenic sources of black carbon, although distributed globally, are most concentrated in the tropics where solar irradiance is highest. Black carbon is often transported over long distances, mixing with other aerosols along the way. The aerosol mix can form transcontinental plumes of atmospheric brown clouds, with vertical extents of 3 to 5 km. Because of the combination of high absorption, a regional distribution roughly aligned with solar irradiance, and the capacity to form widespread atmospheric brown clouds in a mixture with other aerosols, emissions of black carbon are the second strongest contribution to current global warming, after carbon dioxide emissions. In the Himalayan region, solar heating from black carbon at high elevations may be just as important as carbon dioxide in the melting of snowpacks and glaciers. The interception of solar radiation by atmospheric brown clouds leads to dimming at the Earth's surface with important implications for the hydrological cycle, and the deposition of black carbon darkens snow and ice surfaces, which can contribute to melting, in particular of Arctic sea ice.
Details
- Title: Subtitle
- Global and regional climate changes due to black carbon
- Creators
- V Ramanathan - University of California, San DiegoG Carmichael - University of Iowa
- Resource Type
- Journal article
- Publication Details
- Nature geoscience, Vol.1(4), pp.221-227
- Publisher
- Nature Publishing Group
- DOI
- 10.1038/ngeo156
- ISSN
- 1752-0894
- eISSN
- 1752-0908
- Language
- English
- Date published
- 2008
- Academic Unit
- Nursing; Chemical and Biochemical Engineering; Civil and Environmental Engineering
- Record Identifier
- 9984231919302771
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