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...
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Veröffentlicht in: | Journal of Geophysical Research: Oceans 2012-11, Vol.117 (C11), p.n/a |
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container_title | Journal of Geophysical Research: Oceans |
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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 |
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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. 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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> |
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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 |
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