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- W2026196680 abstract "When air blows over a closed channel of water a steady surface velocity develops, as part of a flow extending to the channel bed. With concentrated solutions of surfactants an entirely different flow is produced. The surface velocity us increases with the downwind distance x as us∝x13, and the flow is confined to a boundary layer adjacent to the surface. The boundary layer flow is a new type, but is related to that generated by a solid surface moving through a quiescent fluid. The characteristics of this flow are determined experimentally and theoretically, and the importance of surface tension gradients to its genesis and maintenance is developed." @default.
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- W2026196680 date "1968-06-01" @default.
- W2026196680 modified "2023-09-23" @default.
- W2026196680 title "The interpretation of measurements of the amplitude of capillary waves generated by a wind" @default.
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- W2026196680 doi "https://doi.org/10.1016/0009-2509(68)87015-0" @default.
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