The generation of wind waves on clean water and in the presence of an oil film

2016 ◽  
Vol 71 (1) ◽  
pp. 139-142 ◽  
Author(s):  
O. N. Mel’nikova ◽  
K. V. Pokazeev
Ocean Science ◽  
2019 ◽  
Vol 15 (3) ◽  
pp. 725-743 ◽  
Author(s):  
Alvise Benetazzo ◽  
Luigi Cavaleri ◽  
Hongyu Ma ◽  
Shumin Jiang ◽  
Filippo Bergamasco ◽  
...  

Abstract. Surfactant layers with viscoelastic properties floating on the water surface dampen short gravity-capillary waves. Taking advantage of the known virtue of fish oil to still angry seas, a laboratory study has been made to analyse wind-wave generation and the interaction between wind waves, paddle waves, and airflow. This was done in a tank containing a thin fish-oil film uniformly spread on the water surface. The research was aimed, on the one hand, at quantifying for the first time the effectiveness of this surfactant at impeding the generation of wind waves and, on the other, at using the derived conditions to disentangle relevant mechanisms involved in the air–sea interaction. In particular, our main interest concerned the processes acting on the wind stress and on the wave growth. With oil on the water surface, we have found that in the wind-only condition (no paddle waves) the wave field does not grow from the rest condition. This equilibrium is altered by irregular paddle (long) waves, the generation and evolution of short waves (in clean water and with oil) being modified by their interaction with the orbital velocity of the long waves and their effect on the airflow. Paddle waves do grow under the action of wind, the amount being similar in clean and oily water conditions, a fact we ascribe to the similar distortion of the wind vertical profile in the two cases. We have also verified that the wind-supported stress on the oily water surface was able to generate a surface current, whose magnitude turns out to be comparable to the one in clean water. We stress the benefits of experiments with surfactants to explore in detail the physics at, and the exchanges across, the wavy and non-wavy air–water interface.


2020 ◽  
Vol 24 (1) ◽  
pp. 518-525
Author(s):  
Eshev S.S.– DSc ◽  
I.X. Gayimnazarov ◽  
А.R. Rakhimov ◽  
Latipov Sh. A

2020 ◽  
Vol 8 (8) ◽  
pp. 623
Author(s):  
Christian Kharif ◽  
Malek Abid

The generation of wind waves at the surface of a pre-existing underlying vertically sheared water flow of constant vorticity is considered. Emphasis is put on the role of the vorticity in water on wind-wave generation. The amplitude growth rate increases with the vorticity except for quite old waves. A limit to the wave energy growth is found in the case of negative vorticity, corresponding to the vanishing of the growth rate.


1967 ◽  
Vol 93 (1) ◽  
pp. 105-109
Author(s):  
Otakar W. Kabelac ◽  
Omar H. Shemdin ◽  
En Yun Hsu

1966 ◽  
Vol 92 (2) ◽  
pp. 1-26
Author(s):  
Robert L. Wiegel ◽  
Ralph H. Cross

2018 ◽  
Author(s):  
Alvise Benetazzo ◽  
Luigi Cavaleri ◽  
Hongyu Ma ◽  
Shumin Jiang ◽  
Filippo Bergamasco ◽  
...  

Abstract. Surfactant layers with viscoelastic properties floating on the water surface damp short gravity-capillary waves. Inspired by the known virtue of fish oil to still angry seas, a laboratory study has been made on wind wave generation and on the interaction between wind-waves, paddle-waves and airflow in a tank containing a thin fish oil film uniformly spread on the water surface. According to the Marangoni resonance-type damping mechanism, for oily surfaces the energy dissipation process is quite selective in wavenumbers, but its effects are not, since it spreads (although to a lesser extent) towards longer and shorter waves via nonlinear interactions and modification of the airflow profile. With a thin layer of oil on the surface, it is rather peculiar that in the wind-only condition (no paddle waves) the wave field does not grow from the rest condition. This equilibrium was altered by paddle (longer) waves, the generation and evolution of short waves (in clean water and with oil) being modified by their interaction with the orbital velocity of the longer waves and their effect on the airflow. Paddle waves did grow under the action of wind, how much being similar in clean and oily water conditions, a fact we ascribe to the similar distortion of the wind profile in the two cases. We have also found that wind-supported stress on the oily water surface was able to generate a surface current, whose magnitude turns out to be comparable to the one in clean water. Our results expand previous investigations on the same topic. We stress the benefit of experiments with surfactants to explore in detail the physics at, and the exchanges across, the wavy and no-wavy air-water interface.


2015 ◽  
Vol 12 (4) ◽  
pp. 1291-1325 ◽  
Author(s):  
D. Kiefhaber ◽  
C. J. Zappa ◽  
B. Jähne

Abstract. Results from measurements of wave slope statistics during the R/V Meteor M91 cruise in the coastal upwelling regions off the coast of Peru are reported. Wave slope probability distributions were measured with an instrument based on the reflection of light at the water surface and a method very similar to the Cox and Munk (1954b) sun glitter technique. During the cruise, the mean square slope (mss) of the waves was found to be very variable, despite the limited range of encountered wind speeds. The Cox and Munk (1954b) parameterization for clean water is found to overestimate mss, but most measurements fall in the range spanned by their clean water and slick parameterizations. The observed variability of mss is attributed to the wave damping effect of surface films, generated by increased biological production in the upwelling zones. The small footprint and high temporal resolution of the measurement allows for tracking abrupt changes in conditions caused by the often patchy structure of the surface films.


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