Abstract
Observations of the number and size of the smaller salt particles in the air over Hawaiian and Alaskan seas are presented. Differences in the mean curves representing particle distribution at the two locations are related to differences in the behavior of air bubbles of various sizes near and on a sea water surface. The relationships found suggest that a break in the curves among particles of ∼10−13–10−14 grams marks a zone of transition from a bubble jet to a bubble film source of droplets and that the Alaskan waters are a relatively poor source of particles of <∼10−14 grams.
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