The effect of swell waves on atmospheric boundary layer turbulence under low winds was explored using data from a fixed platform located in the South China Sea. The wind spectra, cospectra, and Ogive curve measured at a height of 8 m above the mean sea surface provided direct evidence that wind stress was affected by swell waves. To interpret such phenomena, an improved approach was derived based on the fact that the total wind stress was the vector sum of turbulent stress and wave‐coherent stress. Different from the approaches of earlier studies, our approach did not align the turbulent stress with the mean wind speed. The influence of swell waves on the magnitude and direction of the total wind stress was analyzed using our approach. The results showed that the wave‐coherent stress derived from our data accounted for 32% of the total wind stress. The magnitude and angle of the wind stress changed by swell waves depended on the relative angle between the turbulent stress and swell direction.

A linear instability analysis of the Taylor-Couette flow between two rotating coaxial cylinders in the presence of the semi-concentrated fibers is performed. Based on the model of an anisotropic fluid described by Erickson, a set of modified stability equations are derived by introducing a small disturbance to the basic flow. The numerical solutions of an eigenvalue problem determining the hydrodynamic instability show that the fiber additives have a stabilizing effect on the flow, and this effect is clearer for higher values of fiber volume fraction, fiber aspect ratio and lower values of two cylinder radius ratio.

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