Abstract
Abstract Shapes of mean water velocity profiles measured with microscopic bubble tracers in developing, laminar flows are recognizably different from those in a turbulent flow. A previously deduced viscous sublayer occurs at the surface, although it is thinner than an analogous sublayer computed for a solid boundary. The differing thickness leads in part to decreased surface temperatures at slicks.
Cite
CITATION STYLE
Mcleish, W., & Putland, G. E. (1975). Measurements of Wind-Driven Flow Profiles in the Top Millimeter of Water. Journal of Physical Oceanography, 5(3), 516–518. https://doi.org/10.1175/1520-0485(1975)005<0516:mowdfp>2.0.co;2
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