Strong radiative heating due to the mixing state of black carbon in atmospheric aerosols
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Summary
Simulation of the evolution of the chemical composition of aerosols finds that the mixing state and direct forcing of the black-carbon component approach those of an internal mixture, largely due to coagulation and growth of aerosol particles.
- Type
- article
- Published
- 2001-02-08
- Cited by
- 2,570
- References
- 53
- OpenAlex
- https://openalex.org/W1560749659
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:4423927
Keywords
Radiative forcing, Aerosol, Soot, Carbon black, Atmospheric sciences
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- Charging and Aggregation Properties of Carboxyl Latex Particles: Experiments versus DLVO Theory
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- Aerosol properties and radiative effects in the United States East Coast haze plume: An overview of the Tropospheric Aerosol Radiative Forcing Observational Experiment (TARFOX)
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- High-pressure transformations in simple melts
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- Response to Comment on "Radiative Absorption Enhancements Due to the Mixing State of Atmospheric Black Carbon"
- Models for integrated and differential scattering optical properties of encapsulated light absorbing carbon aggregates.
- Regional climate effects of internally and externally mixed aerosols over China
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- An overview of the studies on black carbon and mineral dust deposition in snow and ice cores in East Asia
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- Etude structurale et dynamique des fractions lipidiques et organiques réfractaires de sols d'une chronoséquence forêt/maïs (Cestas, sud ouest de la France)
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