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Ice Nucleation Properties of Soil Derived Mineral and Soil Organic Particles

Soil organic and mineral particles are emitted to the atmosphere through recently discovered landatmosphere interactions (e.g., raindrop impaction on soil surface) [1-3]. However, there is, an ongoing debate on whether these aerosols can influence the background atmospheric aerosol budget and further, whether they influence cold cloud formation by acting as ice nucleating particles (INP). Heterogeneous ice nucleation processes and the concentration of INPs influence the formation of ice cloud, thus affecting cloud radiative properties and precipitation. These processes depend upon the physical and chemical properties of INPs, and presently such properties are poorly characterized.