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Surface deformations and wave generation by wind blowing over a viscous liquid
We investigate experimentally the early stage of the generation of waves by a turbulent wind at the surface of a viscous liquid. The spatio-temporal structure of the surface deformation is analyzed by the optical method Free Surface Synthetic Schlieren, which allows for time-resolved measurements wi...
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Published in: | Physics of fluids (1994) 2015-12, Vol.27 (12) |
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container_title | Physics of fluids (1994) |
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creator | Paquier, A. Moisy, F. Rabaud, M. |
description | We investigate experimentally the early stage of the generation of waves by a turbulent wind at the surface of a viscous liquid. The spatio-temporal structure of the surface deformation is analyzed by the optical method Free Surface Synthetic Schlieren, which allows for time-resolved measurements with a micrometric accuracy. Because of the high viscosity of the liquid, the flow induced by the turbulent wind in the liquid remains laminar, with weak surface drift velocity. Two regimes of deformation of the liquid-air interface are identified. In the first regime, at low wind speed, the surface is dominated by rapidly propagating disorganized wrinkles, elongated in the streamwise direction, which correspond to the surface response to the pressure fluctuations advected by the turbulent airflow. The amplitude of these deformations increases approximately linearly with wind velocity and are essentially independent of the fetch (distance along the channel). Above a threshold in wind speed, we observe the growth of well defined gravity-capillary waves with crests nearly perpendicular to the wind direction. In this second regime, the wave amplitude increases with wind speed but far more quickly than in the first regime. |
doi_str_mv | 10.1063/1.4936395 |
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In this second regime, the wave amplitude increases with wind speed but far more quickly than in the first regime.</description><subject>Aerodynamics</subject><subject>Air flow</subject><subject>Amplitudes</subject><subject>Capillary waves</subject><subject>Deformation analysis</subject><subject>Fluid dynamics</subject><subject>Fluid mechanics</subject><subject>Free surfaces</subject><subject>Mechanics</subject><subject>Physics</subject><subject>Turbulent flow</subject><subject>Turbulent wind</subject><subject>Variations</subject><subject>Velocity</subject><subject>Wave generation</subject><subject>Wind direction</subject><subject>Wind speed</subject><issn>1070-6631</issn><issn>1089-7666</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><recordid>eNpFkFFLwzAUhYMoOKcP_oOATz50Jrlp2jyOoU4Y-qA-h9s0nR1dsyVrx_69nQ59OpePw8flEHLL2YQzBQ98IjUo0OkZGXGW6yRTSp0f74wlSgG_JFcxrhhjoIUakdf3LlRoHS1d5cMad7VvI8W2pHvsHV261oUfSIsD3dcDLxo_5JL63gWKtK-j9V2kTb3t6vKaXFTYRHdzyjH5fHr8mM2Txdvzy2y6SCyk2S4pSusQNQhRcCkUAJdYCCUYyhywEmC1ZLqwknOlSis01xYcujKTVmBqYUzuf71f2JhNqNcYDsZjbebThTkyBrlKpRQ9H7p3v91N8NvOxZ1Z-S60w3tGcAFZznOW_xtt8DEGV_1pOTPHaQ03p2nhG2XjadU</recordid><startdate>20151201</startdate><enddate>20151201</enddate><creator>Paquier, A.</creator><creator>Moisy, F.</creator><creator>Rabaud, M.</creator><general>American Institute of Physics</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0003-0408-4232</orcidid><orcidid>https://orcid.org/0000-0003-1527-4744</orcidid></search><sort><creationdate>20151201</creationdate><title>Surface deformations and wave generation by wind blowing over a viscous liquid</title><author>Paquier, A. ; Moisy, F. ; Rabaud, M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c357t-bdceaa9322b14263314ab2620a483af23c9409bc41166dc2919c3eaed74c2a5c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Aerodynamics</topic><topic>Air flow</topic><topic>Amplitudes</topic><topic>Capillary waves</topic><topic>Deformation analysis</topic><topic>Fluid dynamics</topic><topic>Fluid mechanics</topic><topic>Free surfaces</topic><topic>Mechanics</topic><topic>Physics</topic><topic>Turbulent flow</topic><topic>Turbulent wind</topic><topic>Variations</topic><topic>Velocity</topic><topic>Wave generation</topic><topic>Wind direction</topic><topic>Wind speed</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Paquier, A.</creatorcontrib><creatorcontrib>Moisy, F.</creatorcontrib><creatorcontrib>Rabaud, M.</creatorcontrib><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Physics of fluids (1994)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Paquier, A.</au><au>Moisy, F.</au><au>Rabaud, M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Surface deformations and wave generation by wind blowing over a viscous liquid</atitle><jtitle>Physics of fluids (1994)</jtitle><date>2015-12-01</date><risdate>2015</risdate><volume>27</volume><issue>12</issue><issn>1070-6631</issn><eissn>1089-7666</eissn><abstract>We investigate experimentally the early stage of the generation of waves by a turbulent wind at the surface of a viscous liquid. The spatio-temporal structure of the surface deformation is analyzed by the optical method Free Surface Synthetic Schlieren, which allows for time-resolved measurements with a micrometric accuracy. Because of the high viscosity of the liquid, the flow induced by the turbulent wind in the liquid remains laminar, with weak surface drift velocity. Two regimes of deformation of the liquid-air interface are identified. In the first regime, at low wind speed, the surface is dominated by rapidly propagating disorganized wrinkles, elongated in the streamwise direction, which correspond to the surface response to the pressure fluctuations advected by the turbulent airflow. The amplitude of these deformations increases approximately linearly with wind velocity and are essentially independent of the fetch (distance along the channel). Above a threshold in wind speed, we observe the growth of well defined gravity-capillary waves with crests nearly perpendicular to the wind direction. 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source | American Institute of Physics:Jisc Collections:Transitional Journals Agreement 2021-23 (Reading list); AIP Digital Archive |
subjects | Aerodynamics Air flow Amplitudes Capillary waves Deformation analysis Fluid dynamics Fluid mechanics Free surfaces Mechanics Physics Turbulent flow Turbulent wind Variations Velocity Wave generation Wind direction Wind speed |
title | Surface deformations and wave generation by wind blowing over a viscous liquid |
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