Abstract
Giant nuclei (GN) concentrations (N GN) below RICO small cumulus clouds were substantially correlated with drizzle drop concentrations (N d), especially at higher cloud altitudes. The N GN -N d correlation coefficients (R) progressively increased with altitude whereas R for CCN concentrations with N d were negative with mostly decreasing magnitudes at increasing altitudes. These results indicate that the positive influence of GN [or CCN with low critical supersaturations (S c)] on N d is greater than the negative influence of high S c CCN on N d at high cloud altitudes where there are more drizzle drops. This work has implications not only for fundamental cloud physics but also for climate change; i.e., global warming and the indirect aerosol effect as well as geoengineering and hygroscopic cloud seeding. Copyright 2011 by the American Geophysical Union.
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CITATION STYLE
Hudson, J. G., Jha, V., & Noble, S. (2011). Drizzle correlations with giant nuclei. Geophysical Research Letters, 38(5). https://doi.org/10.1029/2010GL046207
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