Laboratory and theoretical modeling of air-sea momentum transfer under severe wind conditions

The laboratory experiments on investigation of aerodynamic resistance of the waved water surface under severe wind conditions (up to U10 ≈ 40 m s−1) were carried out, complemented by measurements of the wind‐wave spectra. The tendency to saturation of the surface drag was observed for wind speeds ex...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of Geophysical Research: Oceans 2012-11, Vol.117 (C11), p.n/a
Hauptverfasser: Troitskaya, Y. I., Sergeev, D. A., Kandaurov, A. A., Baidakov, G. A., Vdovin, M. A., Kazakov, V. I.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page n/a
container_issue C11
container_start_page
container_title Journal of Geophysical Research: Oceans
container_volume 117
creator Troitskaya, Y. I.
Sergeev, D. A.
Kandaurov, A. A.
Baidakov, G. A.
Vdovin, M. A.
Kazakov, V. I.
description The laboratory experiments on investigation of aerodynamic resistance of the waved water surface under severe wind conditions (up to U10 ≈ 40 m s−1) were carried out, complemented by measurements of the wind‐wave spectra. The tendency to saturation of the surface drag was observed for wind speeds exceeding 25 m s−1, accompanied by the saturation of wind‐wave slopes. The effect of surface drag saturation can be explained quantitatively within the quasi‐linear model of the air boundary layer above the waved water surface, when the contribution of the short‐wave part of the wind‐wave spectrum to aerodynamic resistance of the water surface is taken into account. Key Points Laboratory modeling of the air‐sea momentum transfer for hurricane wind Saturation of the aerodynamic drag coefficient Correlation of aerodynamic roughness with mean square slope of the wave field
doi_str_mv 10.1029/2011JC007778
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1919959217</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2801764721</sourcerecordid><originalsourceid>FETCH-LOGICAL-a5380-13e014726d31b19b5ade070a402bc5290fad9a02c1acd4ed11e8a63a8e2997a73</originalsourceid><addsrcrecordid>eNqNkU-LFEEMxQtRcFj35gdo8OLB1iT9p7qOMujoOiiIsl6kyHSntdbuqrWq23W-vSUjIh7EHBIIv_dIeErdR3iMQOYJAeLFFkBr3d1SG8KmLYmAbqsNYN2VQKTvqvOUriBX3bQ14EZ93PMhRF5CPBbsh2L5LCHK4nqeijkMMjn_qQhjwS6WSTjvZvHLOhdLZJ9GicXqh9yTfJMoxY3LHn3wg1tc8OmeujPylOT81zxT758_e7d9Ue7f7F5un-5LbqoOSqwkn6ipHSo8oDk0PAho4Bro0DdkYOTBMFCP3A-1DIjScVtxJ2SMZl2dqYcn3-sYvq6SFju71Ms0sZewJosGjWkM4X-gZLCFtq4pow_-Qq_CGn1-xCJi02mNaDL16ET1MaQUZbTX0c0cjxbB_kzG_plMxqsTfuMmOf6TtRe7t1ukuoKsKk8qlxb5_lvF8YttdaUbe_l6Z9t6Dx8u21eWqh9PWJ0f</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1115877119</pqid></control><display><type>article</type><title>Laboratory and theoretical modeling of air-sea momentum transfer under severe wind conditions</title><source>Wiley-Blackwell AGU Digital Library</source><source>Wiley Online Library Journals Frontfile Complete</source><source>Wiley Online Library Free Content</source><source>Alma/SFX Local Collection</source><creator>Troitskaya, Y. I. ; Sergeev, D. A. ; Kandaurov, A. A. ; Baidakov, G. A. ; Vdovin, M. A. ; Kazakov, V. I.</creator><creatorcontrib>Troitskaya, Y. I. ; Sergeev, D. A. ; Kandaurov, A. A. ; Baidakov, G. A. ; Vdovin, M. A. ; Kazakov, V. I.</creatorcontrib><description>The laboratory experiments on investigation of aerodynamic resistance of the waved water surface under severe wind conditions (up to U10 ≈ 40 m s−1) were carried out, complemented by measurements of the wind‐wave spectra. The tendency to saturation of the surface drag was observed for wind speeds exceeding 25 m s−1, accompanied by the saturation of wind‐wave slopes. The effect of surface drag saturation can be explained quantitatively within the quasi‐linear model of the air boundary layer above the waved water surface, when the contribution of the short‐wave part of the wind‐wave spectrum to aerodynamic resistance of the water surface is taken into account. Key Points Laboratory modeling of the air‐sea momentum transfer for hurricane wind Saturation of the aerodynamic drag coefficient Correlation of aerodynamic roughness with mean square slope of the wave field</description><identifier>ISSN: 0148-0227</identifier><identifier>ISSN: 2169-9275</identifier><identifier>EISSN: 2156-2202</identifier><identifier>EISSN: 2169-9291</identifier><identifier>DOI: 10.1029/2011JC007778</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Boundary layers ; drag coefficient ; Geophysics ; laboratory modelling ; Marine ; marine atmospheric boundary layer ; Momentum transfer ; Oceanography ; Physical oceanography ; strong and huricane wind ; surface waves ; Wind speed</subject><ispartof>Journal of Geophysical Research: Oceans, 2012-11, Vol.117 (C11), p.n/a</ispartof><rights>2012. American Geophysical Union. All Rights Reserved.</rights><rights>Copyright American Geophysical Union 2012</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a5380-13e014726d31b19b5ade070a402bc5290fad9a02c1acd4ed11e8a63a8e2997a73</citedby><cites>FETCH-LOGICAL-a5380-13e014726d31b19b5ade070a402bc5290fad9a02c1acd4ed11e8a63a8e2997a73</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2011JC007778$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2011JC007778$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,11493,27901,27902,45550,45551,46384,46443,46808,46867</link.rule.ids></links><search><creatorcontrib>Troitskaya, Y. I.</creatorcontrib><creatorcontrib>Sergeev, D. A.</creatorcontrib><creatorcontrib>Kandaurov, A. A.</creatorcontrib><creatorcontrib>Baidakov, G. A.</creatorcontrib><creatorcontrib>Vdovin, M. A.</creatorcontrib><creatorcontrib>Kazakov, V. I.</creatorcontrib><title>Laboratory and theoretical modeling of air-sea momentum transfer under severe wind conditions</title><title>Journal of Geophysical Research: Oceans</title><addtitle>J. Geophys. Res</addtitle><description>The laboratory experiments on investigation of aerodynamic resistance of the waved water surface under severe wind conditions (up to U10 ≈ 40 m s−1) were carried out, complemented by measurements of the wind‐wave spectra. The tendency to saturation of the surface drag was observed for wind speeds exceeding 25 m s−1, accompanied by the saturation of wind‐wave slopes. The effect of surface drag saturation can be explained quantitatively within the quasi‐linear model of the air boundary layer above the waved water surface, when the contribution of the short‐wave part of the wind‐wave spectrum to aerodynamic resistance of the water surface is taken into account. Key Points Laboratory modeling of the air‐sea momentum transfer for hurricane wind Saturation of the aerodynamic drag coefficient Correlation of aerodynamic roughness with mean square slope of the wave field</description><subject>Boundary layers</subject><subject>drag coefficient</subject><subject>Geophysics</subject><subject>laboratory modelling</subject><subject>Marine</subject><subject>marine atmospheric boundary layer</subject><subject>Momentum transfer</subject><subject>Oceanography</subject><subject>Physical oceanography</subject><subject>strong and huricane wind</subject><subject>surface waves</subject><subject>Wind speed</subject><issn>0148-0227</issn><issn>2169-9275</issn><issn>2156-2202</issn><issn>2169-9291</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNqNkU-LFEEMxQtRcFj35gdo8OLB1iT9p7qOMujoOiiIsl6kyHSntdbuqrWq23W-vSUjIh7EHBIIv_dIeErdR3iMQOYJAeLFFkBr3d1SG8KmLYmAbqsNYN2VQKTvqvOUriBX3bQ14EZ93PMhRF5CPBbsh2L5LCHK4nqeijkMMjn_qQhjwS6WSTjvZvHLOhdLZJ9GicXqh9yTfJMoxY3LHn3wg1tc8OmeujPylOT81zxT758_e7d9Ue7f7F5un-5LbqoOSqwkn6ipHSo8oDk0PAho4Bro0DdkYOTBMFCP3A-1DIjScVtxJ2SMZl2dqYcn3-sYvq6SFju71Ms0sZewJosGjWkM4X-gZLCFtq4pow_-Qq_CGn1-xCJi02mNaDL16ET1MaQUZbTX0c0cjxbB_kzG_plMxqsTfuMmOf6TtRe7t1ukuoKsKk8qlxb5_lvF8YttdaUbe_l6Z9t6Dx8u21eWqh9PWJ0f</recordid><startdate>201211</startdate><enddate>201211</enddate><creator>Troitskaya, Y. I.</creator><creator>Sergeev, D. A.</creator><creator>Kandaurov, A. A.</creator><creator>Baidakov, G. A.</creator><creator>Vdovin, M. A.</creator><creator>Kazakov, V. I.</creator><general>Blackwell Publishing Ltd</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>201211</creationdate><title>Laboratory and theoretical modeling of air-sea momentum transfer under severe wind conditions</title><author>Troitskaya, Y. I. ; Sergeev, D. A. ; Kandaurov, A. A. ; Baidakov, G. A. ; Vdovin, M. A. ; Kazakov, V. I.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a5380-13e014726d31b19b5ade070a402bc5290fad9a02c1acd4ed11e8a63a8e2997a73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Boundary layers</topic><topic>drag coefficient</topic><topic>Geophysics</topic><topic>laboratory modelling</topic><topic>Marine</topic><topic>marine atmospheric boundary layer</topic><topic>Momentum transfer</topic><topic>Oceanography</topic><topic>Physical oceanography</topic><topic>strong and huricane wind</topic><topic>surface waves</topic><topic>Wind speed</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Troitskaya, Y. I.</creatorcontrib><creatorcontrib>Sergeev, D. A.</creatorcontrib><creatorcontrib>Kandaurov, A. A.</creatorcontrib><creatorcontrib>Baidakov, G. A.</creatorcontrib><creatorcontrib>Vdovin, M. A.</creatorcontrib><creatorcontrib>Kazakov, V. I.</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Journal of Geophysical Research: Oceans</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Troitskaya, Y. I.</au><au>Sergeev, D. A.</au><au>Kandaurov, A. A.</au><au>Baidakov, G. A.</au><au>Vdovin, M. A.</au><au>Kazakov, V. I.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Laboratory and theoretical modeling of air-sea momentum transfer under severe wind conditions</atitle><jtitle>Journal of Geophysical Research: Oceans</jtitle><addtitle>J. Geophys. Res</addtitle><date>2012-11</date><risdate>2012</risdate><volume>117</volume><issue>C11</issue><epage>n/a</epage><issn>0148-0227</issn><issn>2169-9275</issn><eissn>2156-2202</eissn><eissn>2169-9291</eissn><abstract>The laboratory experiments on investigation of aerodynamic resistance of the waved water surface under severe wind conditions (up to U10 ≈ 40 m s−1) were carried out, complemented by measurements of the wind‐wave spectra. The tendency to saturation of the surface drag was observed for wind speeds exceeding 25 m s−1, accompanied by the saturation of wind‐wave slopes. The effect of surface drag saturation can be explained quantitatively within the quasi‐linear model of the air boundary layer above the waved water surface, when the contribution of the short‐wave part of the wind‐wave spectrum to aerodynamic resistance of the water surface is taken into account. Key Points Laboratory modeling of the air‐sea momentum transfer for hurricane wind Saturation of the aerodynamic drag coefficient Correlation of aerodynamic roughness with mean square slope of the wave field</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2011JC007778</doi><tpages>13</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0148-0227
ispartof Journal of Geophysical Research: Oceans, 2012-11, Vol.117 (C11), p.n/a
issn 0148-0227
2169-9275
2156-2202
2169-9291
language eng
recordid cdi_proquest_miscellaneous_1919959217
source Wiley-Blackwell AGU Digital Library; Wiley Online Library Journals Frontfile Complete; Wiley Online Library Free Content; Alma/SFX Local Collection
subjects Boundary layers
drag coefficient
Geophysics
laboratory modelling
Marine
marine atmospheric boundary layer
Momentum transfer
Oceanography
Physical oceanography
strong and huricane wind
surface waves
Wind speed
title Laboratory and theoretical modeling of air-sea momentum transfer under severe wind conditions
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-03T09%3A23%3A23IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Laboratory%20and%20theoretical%20modeling%20of%20air-sea%20momentum%20transfer%20under%20severe%20wind%20conditions&rft.jtitle=Journal%20of%20Geophysical%20Research:%20Oceans&rft.au=Troitskaya,%20Y.%20I.&rft.date=2012-11&rft.volume=117&rft.issue=C11&rft.epage=n/a&rft.issn=0148-0227&rft.eissn=2156-2202&rft_id=info:doi/10.1029/2011JC007778&rft_dat=%3Cproquest_cross%3E2801764721%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1115877119&rft_id=info:pmid/&rfr_iscdi=true