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- W2023176750 startingPage "2747" @default.
- W2023176750 abstract "If above some surface one observes under neutral conditions a logarithmic velocity distribution, it is possible to assign a ‘roughness length’ z0 to the surface using the wellhyphen;known ‘wall layer’ law (see, for example, Monin and Yaglom [1971]): where u* = 7lpar;τ0/ρ)1/2 is friction velocity, k is Karman's constant, and z0 is roughness length. It is in this manner that the roughness of the sea surface has been determined in many observations, notably those summarized by Roll [1965] and those published by Sheppard et al. [1972]. We see that z0 is a parameter describing the flow in the universal (logarithmic) portion of the wall layer, even if its value is determined by processes close to the wall, either in a viscous sublayer or in what one might call a ‘rough sublayer,’ within which the flow is irregular. These processes establish where the edge of the sublayer is and what the velocity is there, providing a lower boundary condition for (1)." @default.
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- W2023176750 date "1974-06-20" @default.
- W2023176750 modified "2023-10-09" @default.
- W2023176750 title "The ‘roughness’ of the sea surface in light winds" @default.
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- W2023176750 doi "https://doi.org/10.1029/jc079i018p02747" @default.
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