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- W2155169102 abstract "Formation of steam fog depends upon the rate of transfer of water vapor at two levels, namely, (1) at the surface of the water, where water vapor is introduced into the lowest layer of the atmosphere, and (2) at the top of the potentially foggy layer, where vapor is removed from the lower air by mixing with drier air aloft. At the former level, transfer is a function of temperature of the water, dewpoint, and the turbulent exchange; at the latter level it is a function of the vapor pressure and turbulent exchange in the air.These rates of transfer depend on four factors, the balance among which determines whether the lower layers of air become saturated and excess water condenses as fog-droplets: (a) The difference between vapor pressures at the water surface and in the lowest layer of air; (b) the difference between vapor pressures in the potentially foggy layer of air and the higher layers; (c) turbulent exchange just above the water surface, and (d) turbulent exchange at higher levels. Introduction of water vapor into the potentially foggy layer depends upon (a) and (c), and its removal upon (b) and (d). The relations among these four factors may be seen when they are brought together into an inequality which must be realized if fog is to be formed." @default.
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- W2155169102 date "1946-01-01" @default.
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- W2155169102 title "Discussion of “Steam fog over Lake Michigan in winter”" @default.
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- W2155169102 doi "https://doi.org/10.1029/tr027i004p00575" @default.
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