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Biomass burning produces light-absorbing aerosol containing a mixture of black carbon (BC) and organic carbon (OC). When OC absorbs more strongly at the blue end of solar spectrum than at the red end, it is called brown carbon (BrC) due to its brownish appearance. The exact configuration of BC and OC within the aerosol is highly variable over geography and time. To represent realistically the radiative properties of such composite aerosols in climate models is not an easy task. Furthermore, the amount and the chemical composition of BrC emitted is unknown and it is often inferred from measured optical properties of mixed carbonaceous aerosols.