A note on a critical wind speed for air-sea boundary processes

作者：Mitsuyasu Hisashi^*

来源：Journal of Oceanography, 2017, 73(2): 169-180.

DOI：10.1007/s10872-016-0394-9

• Air-sea boundary processes
• Critical wind speed
• Sea surface roughness
• Breaking waves
• High frequency wave spectrum

Wind and wind-generated waves were measured in a wind-wave tank. A clear transition was found in the relation between the wind speed U (10) and the wind friction velocity u (*) near u (*) = 0.2 m/s, where U (10) is the wind speed at 10 m height extrapolated from the measured wind profile in a logarithmic layer, and u (*) = 0.2 m/s corresponds roughly to U (10) = 8 m/s in the present measurement. Quite a similar transition was found in the relation between the spectral density of high frequency wind waves and u (*). These results suggest the existence of the critical wind speed for air-sea boundary processes, which was proposed by Munk (J Marine Res 6:203-218, 1947) more than half a century ago. His original idea of the critical wind speed was based on the discontinuities in such phenomena as white caps, wind stress, and evaporation, which commonly appear at a wind speed near 7 m/s. On the basis of the results of our present study and those of earlier studies, we discuss the phenomena which are relevant to the critical wind speed for the air-sea boundary processes. The conclusion is that the critical wind speed exists and it is attributed to the start of wave breaking rather than the Kelvin-Helmholtz instability, but the air-sea boundary processes are not discontinuous at a particular wind speed; because of the stochastic nature of breaking waves, the changes occur over a range of wind speeds. Detailed discussions are presented on the dynamical processes associated with the critical wind speed such as wind-induced change of sea surface roughness and high frequency wave spectrum. Future studies are required, however, to clarify the dynamical processes quantitatively. In particular, there is a need to further examine the gradual change of breaking patterns of wind waves with the increase of wind speed, and the associated change of the structure of the wind over wind waves, such as separation of the airflow at the crest of wind waves, the turbulent stress, and wave-induced stress. Studies on the dynamical structure of the high frequency wave spectrum are also needed.

• 出版日期2017-4