American Association for Aerosol Research - Abstract Submission

AAAR 37th Annual Conference
October 14 - October 18, 2019
Oregon Convention Center
Portland, Oregon, USA

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What Matters for the Climate Impact of Biomass Burning Smoke

DANIEL MURPHY, NOAA ESRL

     Abstract Number: 306
     Working Group: Biomass Combustion: Emissions, Chemistry, Air Quality, Climate, and Human Health

Abstract
Biomass burning smoke is one of the largest and most diverse sources of aerosol in the atmosphere. I will provide an overview of how the radiative properties of smoke affect climate. If there is one message it is that simple radiative transfer calculations do not capture the climate impact of black or brown carbon. The concept of “adjusted radiative forcing” is crucial to understanding the climate impact of smoke. Even the sign can change: in some locations black carbon cools the Earth. Smoke is neither purely scattering nor black, it has multiple light-absorbing species, and is often injected above the surface. Each of these properties of smoke can have important implications for the radiative impacts. For example, altitude affects the radiative impact of an absorbing aerosol much more than it affects a purely scattering aerosol. That implies that the same smoke, containing both scattering and absorbing aerosol, can be net cooling if it is at one altitude and net warming at another.