Loading…

INTERACTION OF WIND WITH SURFACE WATER WAVES

A turbulent flow over different growing and non growing water waves is considered by constructing a high-Reynolds-number stress closure model. The profile of the water wave as well as the associated orbital velocities are prescribed. In the case of a growing wave, the profile and the orbital velocit...

Full description

Saved in:
Bibliographic Details
Published in:Neural, parallel & scientific computations parallel & scientific computations, 2014-09, Vol.22 (3), p.303-314
Main Authors: DRULLION, F, Sajjadi, S G
Format: Article
Language:English
Subjects:
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by
cites
container_end_page 314
container_issue 3
container_start_page 303
container_title Neural, parallel & scientific computations
container_volume 22
creator DRULLION, F
Sajjadi, S G
description A turbulent flow over different growing and non growing water waves is considered by constructing a high-Reynolds-number stress closure model. The profile of the water wave as well as the associated orbital velocities are prescribed. In the case of a growing wave, the profile and the orbital velocities can change dynamically under the action of the wind blowing above the wave. This work focuses on the influence of the wave age (ratio of the wave speed over the wall friction velocity) and the wave steepness on the dynamics of the critical layer (the region about the height at which the real part of the complex wave phase speed is equal to the mean flow velocity) and on region of close streamlines, called cat's eye patterns that are created above the surface of the wave and is centered about the critical layer. The simulations show that the height of the critical layer increases with the wave age and the steepness of the wave, what is in agreement with the direct numerical simulations reported by Sullivan et al.[21]. The cat's eye patterns increase in size and extend vertically with the increase of the wave age and lead to a maximum disturbance of the mean flow for older waves. The model being computationally less expensive than a DNS approach, it allowed us to study waves growing under the influence of the wind. The simulations show that as the wave grows the critical layer elevates and the cat's eye structures become larger leading again to an important disturbance of the wind flow above the wave.
format article
fullrecord <record><control><sourceid>proquest</sourceid><recordid>TN_cdi_proquest_miscellaneous_1786167747</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1786167747</sourcerecordid><originalsourceid>FETCH-LOGICAL-p103t-462ae16a2325843c38b7391d22542a51c36e46c5096db3f411ea06b1c014a4df3</originalsourceid><addsrcrecordid>eNotjMtqwzAQAHVoIY_mH3zsoQatdrWyj8axG0OwIXGaY5BlGVrcPKrk_2toLzOXYZ7EHCRDrJHTmViE8CUlAhkzF29V3Ra7LG-rpo6aMjpW9XpCu4n2h12Z5UV0zKZg4kexfxHPgx2DX_17KQ5l0eabeNu8V3m2ja8g8R4TK-uBrUKlE0KHSWcwhV4pTcpqcMie2GmZct_hQADeSu7ASSBL_YBL8fr3vf5cbg8f7qfvz-D8ONqzvzzCCUzCwMaQwV_4FTmE</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1786167747</pqid></control><display><type>article</type><title>INTERACTION OF WIND WITH SURFACE WATER WAVES</title><source>EZB Electronic Journals Library</source><creator>DRULLION, F ; Sajjadi, S G</creator><creatorcontrib>DRULLION, F ; Sajjadi, S G</creatorcontrib><description>A turbulent flow over different growing and non growing water waves is considered by constructing a high-Reynolds-number stress closure model. The profile of the water wave as well as the associated orbital velocities are prescribed. In the case of a growing wave, the profile and the orbital velocities can change dynamically under the action of the wind blowing above the wave. This work focuses on the influence of the wave age (ratio of the wave speed over the wall friction velocity) and the wave steepness on the dynamics of the critical layer (the region about the height at which the real part of the complex wave phase speed is equal to the mean flow velocity) and on region of close streamlines, called cat's eye patterns that are created above the surface of the wave and is centered about the critical layer. The simulations show that the height of the critical layer increases with the wave age and the steepness of the wave, what is in agreement with the direct numerical simulations reported by Sullivan et al.[21]. The cat's eye patterns increase in size and extend vertically with the increase of the wave age and lead to a maximum disturbance of the mean flow for older waves. The model being computationally less expensive than a DNS approach, it allowed us to study waves growing under the influence of the wind. The simulations show that as the wave grows the critical layer elevates and the cat's eye structures become larger leading again to an important disturbance of the wind flow above the wave.</description><identifier>ISSN: 1061-5369</identifier><language>eng</language><subject>Age ; Computation ; Computer simulation ; Disturbances ; Orbital velocity ; Steepness ; Surface water ; Water waves</subject><ispartof>Neural, parallel &amp; scientific computations, 2014-09, Vol.22 (3), p.303-314</ispartof><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784</link.rule.ids></links><search><creatorcontrib>DRULLION, F</creatorcontrib><creatorcontrib>Sajjadi, S G</creatorcontrib><title>INTERACTION OF WIND WITH SURFACE WATER WAVES</title><title>Neural, parallel &amp; scientific computations</title><description>A turbulent flow over different growing and non growing water waves is considered by constructing a high-Reynolds-number stress closure model. The profile of the water wave as well as the associated orbital velocities are prescribed. In the case of a growing wave, the profile and the orbital velocities can change dynamically under the action of the wind blowing above the wave. This work focuses on the influence of the wave age (ratio of the wave speed over the wall friction velocity) and the wave steepness on the dynamics of the critical layer (the region about the height at which the real part of the complex wave phase speed is equal to the mean flow velocity) and on region of close streamlines, called cat's eye patterns that are created above the surface of the wave and is centered about the critical layer. The simulations show that the height of the critical layer increases with the wave age and the steepness of the wave, what is in agreement with the direct numerical simulations reported by Sullivan et al.[21]. The cat's eye patterns increase in size and extend vertically with the increase of the wave age and lead to a maximum disturbance of the mean flow for older waves. The model being computationally less expensive than a DNS approach, it allowed us to study waves growing under the influence of the wind. The simulations show that as the wave grows the critical layer elevates and the cat's eye structures become larger leading again to an important disturbance of the wind flow above the wave.</description><subject>Age</subject><subject>Computation</subject><subject>Computer simulation</subject><subject>Disturbances</subject><subject>Orbital velocity</subject><subject>Steepness</subject><subject>Surface water</subject><subject>Water waves</subject><issn>1061-5369</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNotjMtqwzAQAHVoIY_mH3zsoQatdrWyj8axG0OwIXGaY5BlGVrcPKrk_2toLzOXYZ7EHCRDrJHTmViE8CUlAhkzF29V3Ra7LG-rpo6aMjpW9XpCu4n2h12Z5UV0zKZg4kexfxHPgx2DX_17KQ5l0eabeNu8V3m2ja8g8R4TK-uBrUKlE0KHSWcwhV4pTcpqcMie2GmZct_hQADeSu7ASSBL_YBL8fr3vf5cbg8f7qfvz-D8ONqzvzzCCUzCwMaQwV_4FTmE</recordid><startdate>20140901</startdate><enddate>20140901</enddate><creator>DRULLION, F</creator><creator>Sajjadi, S G</creator><scope>7SC</scope><scope>8FD</scope><scope>JQ2</scope><scope>L7M</scope><scope>L~C</scope><scope>L~D</scope></search><sort><creationdate>20140901</creationdate><title>INTERACTION OF WIND WITH SURFACE WATER WAVES</title><author>DRULLION, F ; Sajjadi, S G</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p103t-462ae16a2325843c38b7391d22542a51c36e46c5096db3f411ea06b1c014a4df3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Age</topic><topic>Computation</topic><topic>Computer simulation</topic><topic>Disturbances</topic><topic>Orbital velocity</topic><topic>Steepness</topic><topic>Surface water</topic><topic>Water waves</topic><toplevel>online_resources</toplevel><creatorcontrib>DRULLION, F</creatorcontrib><creatorcontrib>Sajjadi, S G</creatorcontrib><collection>Computer and Information Systems Abstracts</collection><collection>Technology Research Database</collection><collection>ProQuest Computer Science Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Computer and Information Systems Abstracts – Academic</collection><collection>Computer and Information Systems Abstracts Professional</collection><jtitle>Neural, parallel &amp; scientific computations</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>DRULLION, F</au><au>Sajjadi, S G</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>INTERACTION OF WIND WITH SURFACE WATER WAVES</atitle><jtitle>Neural, parallel &amp; scientific computations</jtitle><date>2014-09-01</date><risdate>2014</risdate><volume>22</volume><issue>3</issue><spage>303</spage><epage>314</epage><pages>303-314</pages><issn>1061-5369</issn><abstract>A turbulent flow over different growing and non growing water waves is considered by constructing a high-Reynolds-number stress closure model. The profile of the water wave as well as the associated orbital velocities are prescribed. In the case of a growing wave, the profile and the orbital velocities can change dynamically under the action of the wind blowing above the wave. This work focuses on the influence of the wave age (ratio of the wave speed over the wall friction velocity) and the wave steepness on the dynamics of the critical layer (the region about the height at which the real part of the complex wave phase speed is equal to the mean flow velocity) and on region of close streamlines, called cat's eye patterns that are created above the surface of the wave and is centered about the critical layer. The simulations show that the height of the critical layer increases with the wave age and the steepness of the wave, what is in agreement with the direct numerical simulations reported by Sullivan et al.[21]. The cat's eye patterns increase in size and extend vertically with the increase of the wave age and lead to a maximum disturbance of the mean flow for older waves. The model being computationally less expensive than a DNS approach, it allowed us to study waves growing under the influence of the wind. The simulations show that as the wave grows the critical layer elevates and the cat's eye structures become larger leading again to an important disturbance of the wind flow above the wave.</abstract><tpages>12</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1061-5369
ispartof Neural, parallel & scientific computations, 2014-09, Vol.22 (3), p.303-314
issn 1061-5369
language eng
recordid cdi_proquest_miscellaneous_1786167747
source EZB Electronic Journals Library
subjects Age
Computation
Computer simulation
Disturbances
Orbital velocity
Steepness
Surface water
Water waves
title INTERACTION OF WIND WITH SURFACE WATER WAVES
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-10T16%3A32%3A22IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=INTERACTION%20OF%20WIND%20WITH%20SURFACE%20WATER%20WAVES&rft.jtitle=Neural,%20parallel%20&%20scientific%20computations&rft.au=DRULLION,%20F&rft.date=2014-09-01&rft.volume=22&rft.issue=3&rft.spage=303&rft.epage=314&rft.pages=303-314&rft.issn=1061-5369&rft_id=info:doi/&rft_dat=%3Cproquest%3E1786167747%3C/proquest%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-p103t-462ae16a2325843c38b7391d22542a51c36e46c5096db3f411ea06b1c014a4df3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=1786167747&rft_id=info:pmid/&rfr_iscdi=true