Distant origins of Arctic black carbon: A Goddard Institute for Space Studies ModelE experiment

By D. Koch, J. Hansen. 2005

306 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/37461b8c0cb53be924f90b31ac0a099b9b114f9d

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Citations in the corpus

Single‐particle measurements of midlatitude black carbon and light‐scattering aerosols from the boundary layer to the lower stratosphere (2006, background): “The contribution of BCA to radiative forcing is significant because BCA absorbs light efficiently and accumulates in the atmosphere [Ogren et al., 1984; Cooke and Wilson, 1996; Sato et al., 2003; Penner et al., 1992; Jacobson, 2000; Chung and Seinfeld, 2005; Koch and Hansen, 2005].”
Coatings and their enhancement of black carbon light absorption in the tropical atmosphere (2008, background): “…the most significant particulate absorber of solar radiation in the atmosphere and an important contributor to both globaland regional-scale climate forcing [Chylek et al., 1984; Ramanathan et al., 2001; Jacobson, 2004, 2006; Koch and Hansen, 2005; Chung and Seinfeld, 2005; Tripathi et al., 2005].”
Constraining the magnitude of the global dust cycle by minimizing the difference between a model and observations (2006, methodology): “To address this contribution by other species we use output from a multi-component aerosol model that calculates the distribution of sulfate, sea salt, black and organic carbon [Koch, 2001; Koch et al., 2006; Koch and Hansen, 2005].”
Efficacy of climate forcings (2005, background): “This subdivision is based in part on tracer transport calculations [Koch and Hansen, 2005] in which the sources of soot deposited in the Arctic and other regions were tracked.”
Aerosol light absorption and its measurement: A review (2009, background): “Atmospheric lifetimes are on the order of a eight days [200] and both wet and dry deposition may be important sinks for atmospheric BC [15,16,201].”