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• W2056574532 startingPage "18269" @default.
• W2056574532 abstract "Sea spray in the atmospheric layer near the sea surface was measured by several investigators (Monahan, 1968; Preobrazhenskii, 1973; Wu et al., 1984; de Leeuw, 1986). Their data, obtained at various elevations under different wind velocities, are shown to be generally complementary and are herewith analyzed toward deducing a general description of sea spray. Size spectra are shown to follow an exponential distribution for small droplets and a power law distribution for large droplets. The droplet concentration increases exponentially with the wind velocity, and the production rate of droplets decreases as their size increases. Both numerical and volumetric concentrations of droplets increase with the wind velocity, following a power law; its exponent is greater for volumetric than for numerical concentrations. The droplet has a maximum average size above the sea surface, falling in the range of 15–20 μm. Both numerical and volumetric concentrations decrease exponentially toward higher elevations; the length scale characterizing the decrease of volumetric concentrations is about one half that characterizing numerical concentrations." @default.
• W2056574532 created "2016-06-24" @default.
• W2056574532 creator A5033360196 @default.
• W2056574532 date "1990-10-15" @default.
• W2056574532 modified "2023-10-14" @default.
• W2056574532 title "On parameterization of sea spray" @default.
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• W2056574532 doi "https://doi.org/10.1029/jc095ic10p18269" @default.
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