Image at right: Natural and anthropogenic biomass burning, such as forest fires and the burning of fields in the tropics,
produce black carbon aerosols, i.e., soot.
Not exact matches
Black carbon aerosol deposited on snow has reduced the surface albedo,
producing an associated RF of +0.1 [± 0.1] W m — 2, with a low level of scientific understanding.
Some
aerosols, such as
black carbon, absorb sunlight and
produce a warming effect that might also inhibit rainfall.
They
produce aerosols yes, but a lot of them are
black carbon (a warming influence), and they also
produce NOx, CO and CH4 (ozone precursors) as well as CO2 of course.
In Europe, for instance, the use of coal for power generation
produces very little sulphate
aerosol or
black carbon because of existing air - quality controls.
The
aerosol plume
produced by biomass burning at the end of the dry season contains
black carbon that absorbs radiation.