Radiative Absorption Enhancements Due to the Mixing State of Atmospheric Black Carbon

Autor: R. Subramanian, Chen Song, Paola Massoli, Christopher D. Cappa, Douglas R. Worsnop, Daniel Mellon, Jason S. Olfert, Timothy B. Onasch, I. Nuaaman, Timothy S. Bates, Shao-Meng Li, Katheryn R. Kolesar, Daniel A. Lack, B. Tom Jobson, Paul Davidovits, Jani Hakala, Rahul A. Zaveri, Brian M. Lerner, Eben S. Cross, Katherine Hayden, Patricia K. Quinn, Eric J. Williams, Tuukka Petäjä
Rok vydání: 2012
Předmět:
Zdroj: Cappa, C D, Onasch, T B, Massoli, P, Worsnop, D R, Bates, T S, Cross, E S, Davidovits, P, Hakala, J, Hayden, K L, Jobson, B T, Kolesar, K R, Lack, D A, Lerner, B M, Li, S M, Mellon, D, Nuaaman, I, Olfert, J S, Petäjä, T, Quinn, P K, Song, C, Subramanian, R, Williams, E J & Zaveri, R A 2012, ' Radiative absorption enhancements due to the mixing state of atmospheric black carbon ', Science, vol. 337, no. 6098, pp. 1078-1081 . https://doi.org/10.1126/science.1223447
ISSN: 1095-9203
0036-8075
DOI: 10.1126/science.1223447
Popis: Dark Forcing Soot, or black carbon, is a ubiquitous atmospheric pollutant whose warming effect might be second only to carbon dioxide. When black carbon is emitted, it combines with other aerosols to form heterogeneous mixtures. Models have predicted that internal mixing of black carbon with other materials can double the amount of radiation absorbed. Cappa et al. (p. 1078 ) report that in situ measurements of the enhancement of radiation absorption by these mixed black carbon–containing particles in the atmosphere show a much smaller effect. Thus, many climate models may be overestimating the amount of warming caused by black carbon emissions.
Databáze: OpenAIRE