Microspectroscopic imaging and characterization of individually identified ice nucleating particles from a case field study

• Published in: Journal of geophysical research. Atmospheres 2014-09, Vol.119 (17), p.10,365-10,381
• Main Authors: Knopf, D. A., Alpert, P. A., Wang, B., O'Brien, R. E., Kelly, S. T., Laskin, A., Gilles, M. K., Moffet, R. C.
• Format: Article
• Language: English
• Subjects: aerosol; Anthropogenic factors; Atmospherics; Atoms & subatomic particles; Clouds; Deposition; ENVIRONMENTAL SCIENCES; Freezing; Geophysics; Glaciation; Ice; Ice formation; ice nucleation; Ice nuclei; Light microscopy; Marine; Nucleation; organic aerosol; Physicochemical properties; Surface area; Water uptake
• ISSN: 2169-897X; 2169-8996
• DOI: 10.1002/2014JD021866

The effect of anthropogenic and biogenic organic particles on atmospheric glaciation processes is poorly understood. We use an optical microscopy setup to identify the ice nuclei (IN) active in immersion freezing (IMF) and deposition ice nucleation within a large population of particles collected on a substrate from an ambient environment in central California dominated by urban and marine aerosols. Multimodal microspectroscopy methods are applied to characterize the physicochemical properties and mixing state of the individual IN and particle populations to identify particle‐type classes. The temperature onsets of water uptake occurred between 235 and 257 K at subsaturated conditions, and the onsets of IMF proceeded at subsaturated and saturated conditions for 235–247 K, relevant for ice nucleation in mixed‐phase clouds. Particles also took up water and nucleated ice between 226 and 235 K and acted as deposition IN with onset temperatures below 226 K, a temperature range relevant to cirrus cloud formation. The identified IN belong to the most common particle‐type classes observed in the field samples: organic coated sea salt and Na‐rich, secondary, and refractory carbonaceous particles. Based on these observations, we suggest that the IN are not always particles with unique chemical composition and exceptional ice nucleation propensity; rather, they are common particles in the ambient particle population. The results suggest that particle‐type abundance and total particle surface area are also crucial factors, in addition to particle‐type ice nucleation efficiency, in determining ice formation within the particle population. Key Points Multimodal microspectroscopy allows the characterization of individual ice nucleiIce nuclei are not exceptional but represent common particle‐type classes in airIce nuclei cloud cycling and surface area are crucial for ice cloud prediction