A large international field experiment and use of transport modeling has yielded physical, chemical, and radiative properties of the abundant aerosols originating from Asia.
No other region on Earth is as large and diverse a source of aerosols (and trace gases) as the Asian continent. In spring, when storm and frontal activity in Asia is most prevalent, industrial pollution, biomass burning, and mineral dust outflows produce an extraordinarily complex regional aerosol mix, composed of inorganic compounds (such as salts of sulfates and nitrates), organic carbon (OC), black carbon (BC or soot), mineral dust, and water. Yet there are few data on the chemical, physical, and optical …
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