Novakov, T., V. Ramanathan, J.E. Hansen, T.W. Kirchstetter, M. Sato, J.E. Sinton, and J.A. Satahye, 2003: Large historical changes of fossil -
fuel black carbon aerosols.
Not exact matches
Black carbon aerosols — particles of
carbon that rise into the atmosphere when biomass, agricultural waste, and fossil
fuels are burned in an incomplete way — are important for understanding climate change, as they absorb sunlight, leading to higher atmospheric temperatures, and can also coat Arctic snow with a darker layer, reducing its reflectivity and leading to increased melting.
In the past, numerous studies have identified
black carbon aerosols emitted from combustion of fossil
fuels and residential biofuels as the dominant light - absorbing
aerosol over South Asia.
«Chiefly the burning of fossil
fuels», not CO2, just burning of fossil
fuels, so
black carbon, indirect
aerosol effects, land use anything that involves the burning of fossil
fuels.
BC FF is for
black carbon from fossil
fuel and biofuel, POA FF is for primary organic
aerosol from fossil
fuel and biofuel, BB is for biomass burning
aerosols and SOA is for secondary organic
aerosols.»
Black carbon and other
aerosols, also emitted during combustion of diesel and marine oil
fuels, are relatively short ‐ lived radiative forcers compared with
carbon dioxide and their reduction is emerging as a key strategy for mitigation.
As stated earlier, I agree with the point that tropospheric
aerosols from fossil
fuels are incredibly bad for human health and other environmental impacts (
black carbon soot, acid rain, radioactive emissions, mercury poisoning), putting us in a situation of damned if we do, damned if we don't.
However, sulphate is invariably internally and externally mixed to varying degrees with other compounds such as biomass burning
aerosol (e.g., Formenti et al., 2003), fossil
fuel black carbon (e.g., Russell and Heintzenberg, 2000), organic
carbon (Novakov et al., 1997; Brock et al., 2004), mineral dust (e.g., Huebert et al., 2003) and nitrate
aerosol (e.g., Schaap et al., 2004).
Organic
carbon aerosol from fossil
fuel sources is invariably internally and externally mixed to some degree with other combustion products such as sulphate and
black carbon (e.g., Novakov et al., 1997; Ramanathan et al., 2001b).