Publication Date:
1985-12-01
Description:
The generation and growth of gravity—capillary waves (A « 1 cm) by wind are reconsidered using linear instability theory to describe the process. For all friction velocities we solve the resulting Orr—Sommerfeld equation using asymptoticmethods. New elements in our theory, compared with the work of Benjamin (1959) andMiles (1962), aremore stress onmathematical rigour and the incorporation of the wind-induced shear current. We find that the growth rate of the initial wavelets, the first waves to be generated by the wind, is proportional to u. We also study the effect of changes in the shape of the profiles of wind and wind-induced current. In doing this we compare results ofMiles (1962), Larson & Wright (1975), Valenzuela (1976), Kawai (1979), Plant & Wright (1980) and our study. We find that the growth rate is very sensitive to the shape of the wind profile while the influence of changes in the current profile ismuch smaller. To determine correctly the phase velocity, the value of current and current shear at the interface are very important,muchmore so than the shape of either wind or current profile. © 1985, Cambridge University Press. All rights reserved.
Print ISSN:
0022-1120
Electronic ISSN:
1469-7645
Topics:
Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
,
Physics
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