Cloud condensation nucleus (CCN) spectral data are presented for the Arctic in spring, which considerably augment the existing meager CCN database for the Arctic. Concurrent measurements of sulfate mass suggest that most of the CCN were commonly not sulfate. Sulfate was more closely associated with particles below the CCN size range. Some measurements of the microphysical structure of Arctic stratus clouds are also described. -Authors
CITATION STYLE
Hegg, D. A., Ferek, R. J., & Hobbs, P. V. (1995). Cloud condensation nuclei over the Arctic Ocean in early spring. Journal of Applied Meteorology, 34(9), 2076–2082. https://doi.org/10.1175/1520-0450(1995)034<2076:CCNOTA>2.0.CO;2
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