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Introduction to Climate and Environmental Physics HS 2014 Lecture IV Christoph Raible, Markus Leuenberger, Fortunat Joos and Thomas Stocker
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Definition Aerosol is a colloid or mixture of fine solid particles and/or liquid droplets in a carrier gas. The particles/ droplets have diameters of 10 -3 μm to >100 μm.
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Annual fluxes of the most important aerosol sources. From Seinfeld and Pandis (2006)2006
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Global source distribution Stier et al. (2005)
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Movie
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Dependence of various scattering processes on the diameter of the particle that leads to scattering and the wavelength of the incident light
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«Dimming and Brightening»
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Wild et al. (2005)
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«Dimming and Brightening» Wild et al. (2005)
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«Dimming and Brightening» Wild et al. (2007)
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Production of sea salt aerosol by bubble bursting (left) and of mineral dust aerosol by saltation (right).
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Oxidation of SO 2 with OH to sulfuric acid
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Idealized volume size distribution of an aged particle.
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Balance of gravity and Stoke’s force for a sphere falling through a medium
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Conceptual view of the aerosol depletion in an air column away from its source by dry deposition wet deposition
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Schematic of various processes leading to extinction and scattering of incoming shortwave radiation
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Elemental composition of different rocks, soil, shale and continental aerosol (Warneck, 1987)Warneck, 1987
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Chemical composition of sea water. From Seinfeld and Pandis (2006).2006
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