The change characteristics of the calculated wind wave fields near lateral boundaries with SWAN model
Since the wind wave model Simulating Waves Nearshore （SWAN） cannot effectively simulate the wave fields near the lateral boundaries, the change characteristics and the distortion ranges of calculated wave factors including wave heights, periods, directions, and lengths near the lateral boundaries of...
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| Veröffentlicht in: | Acta oceanologica Sinica 2016, Vol.35 (1), p.96-105 |
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| creator | Zhang, Hongsheng Zhao, Jiachen Li, Penghui Yue, Wenhan Wang, Zhenxiang |
| description | Since the wind wave model Simulating Waves Nearshore （SWAN） cannot effectively simulate the wave fields near the lateral boundaries, the change characteristics and the distortion ranges of calculated wave factors including wave heights, periods, directions, and lengths near the lateral boundaries of calculation domain are carefully studied in the case of different water depths and wind speeds respectively. The calculation results show that the effects of the variety of water depth and wind speed on the modeled different wave factors near the lateral boundaries are different. In the case of a certain wind speed, the greater the water depth is, the greater the distortion range is. In the case of a certain water depth, the distortion ranges defined by the relative errors of wave heights, periods, and lengths are different from those defined by the absolute errors of the corresponding wave factors. Moreover, the distortion ranges defined by the relative errors decrease with the increase of wind speed; whereas the distortion ranges defined by the absolute errors change a little with the variety of wind speed. The distortion range of wave direction decreases with the increase of wind speed. The calculated wave factors near the lateral boundaries with the SWAN model in the actual physical areas, such as Lake Taihu and Lake Dianshan considered in this study, are indeed distorted if the calculation domains are not enlarged on the basis of actual physical areas. Therefore, when SWAN is employed to calculate the wind wave fields near the shorelines of sea or inland lakes, the appropriate approaches must be adopted to reduce the calculation errors. |
| doi_str_mv | 10.1007/s13131-016-0800-6 |
| format | Article |
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The calculation results show that the effects of the variety of water depth and wind speed on the modeled different wave factors near the lateral boundaries are different. In the case of a certain wind speed, the greater the water depth is, the greater the distortion range is. In the case of a certain water depth, the distortion ranges defined by the relative errors of wave heights, periods, and lengths are different from those defined by the absolute errors of the corresponding wave factors. Moreover, the distortion ranges defined by the relative errors decrease with the increase of wind speed; whereas the distortion ranges defined by the absolute errors change a little with the variety of wind speed. The distortion range of wave direction decreases with the increase of wind speed. The calculated wave factors near the lateral boundaries with the SWAN model in the actual physical areas, such as Lake Taihu and Lake Dianshan considered in this study, are indeed distorted if the calculation domains are not enlarged on the basis of actual physical areas. Therefore, when SWAN is employed to calculate the wind wave fields near the shorelines of sea or inland lakes, the appropriate approaches must be adopted to reduce the calculation errors.</description><identifier>ISSN: 0253-505X</identifier><identifier>EISSN: 1869-1099</identifier><identifier>DOI: 10.1007/s13131-016-0800-6</identifier><language>eng</language><publisher>Beijing: The Chinese Society of Oceanography</publisher><subject>Boundaries ; Climatology ; Distortion ; Earth and Environmental Science ; Earth Sciences ; Ecology ; Engineering Fluid Dynamics ; Environmental Chemistry ; Errors ; Inland waters ; Lakes ; Marine ; Marine & Freshwater Sciences ; Oceanography ; Water depth ; Wave direction ; Wave height ; Wave power ; Wind ; Wind speed ; Wind waves ; 侧边界 ; 天鹅 ; 模型模拟 ; 特征和 ; 相对误差 ; 绝对误差 ; 计算域 ; 风场</subject><ispartof>Acta oceanologica Sinica, 2016, Vol.35 (1), p.96-105</ispartof><rights>The Chinese Society of Oceanography and Springer-Verlag Berlin Heidelberg 2016</rights><rights>The Chinese Society of Oceanography and Springer-Verlag Berlin Heidelberg 2016.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c388t-ee85b860c7e7394056a7c3891a9595521222d66d04fe52374f2279d54c4d19e73</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/86790X/86790X.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s13131-016-0800-6$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2919609395?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,780,784,4024,21388,27923,27924,27925,33744,33745,41488,42557,43805,51319,64385,64387,64389,72469</link.rule.ids></links><search><creatorcontrib>Zhang, Hongsheng</creatorcontrib><creatorcontrib>Zhao, Jiachen</creatorcontrib><creatorcontrib>Li, Penghui</creatorcontrib><creatorcontrib>Yue, Wenhan</creatorcontrib><creatorcontrib>Wang, Zhenxiang</creatorcontrib><title>The change characteristics of the calculated wind wave fields near lateral boundaries with SWAN model</title><title>Acta oceanologica Sinica</title><addtitle>Acta Oceanol. Sin</addtitle><addtitle>Acta Oceanologica Sinica</addtitle><description>Since the wind wave model Simulating Waves Nearshore （SWAN） cannot effectively simulate the wave fields near the lateral boundaries, the change characteristics and the distortion ranges of calculated wave factors including wave heights, periods, directions, and lengths near the lateral boundaries of calculation domain are carefully studied in the case of different water depths and wind speeds respectively. The calculation results show that the effects of the variety of water depth and wind speed on the modeled different wave factors near the lateral boundaries are different. In the case of a certain wind speed, the greater the water depth is, the greater the distortion range is. In the case of a certain water depth, the distortion ranges defined by the relative errors of wave heights, periods, and lengths are different from those defined by the absolute errors of the corresponding wave factors. Moreover, the distortion ranges defined by the relative errors decrease with the increase of wind speed; whereas the distortion ranges defined by the absolute errors change a little with the variety of wind speed. The distortion range of wave direction decreases with the increase of wind speed. The calculated wave factors near the lateral boundaries with the SWAN model in the actual physical areas, such as Lake Taihu and Lake Dianshan considered in this study, are indeed distorted if the calculation domains are not enlarged on the basis of actual physical areas. Therefore, when SWAN is employed to calculate the wind wave fields near the shorelines of sea or inland lakes, the appropriate approaches must be adopted to reduce the calculation errors.</description><subject>Boundaries</subject><subject>Climatology</subject><subject>Distortion</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecology</subject><subject>Engineering Fluid Dynamics</subject><subject>Environmental Chemistry</subject><subject>Errors</subject><subject>Inland waters</subject><subject>Lakes</subject><subject>Marine</subject><subject>Marine & Freshwater Sciences</subject><subject>Oceanography</subject><subject>Water depth</subject><subject>Wave direction</subject><subject>Wave height</subject><subject>Wave power</subject><subject>Wind</subject><subject>Wind speed</subject><subject>Wind waves</subject><subject>侧边界</subject><subject>天鹅</subject><subject>模型模拟</subject><subject>特征和</subject><subject>相对误差</subject><subject>绝对误差</subject><subject>计算域</subject><subject>风场</subject><issn>0253-505X</issn><issn>1869-1099</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kc1O3TAQha2qSL2FPkB3VlnAJjC2YzteIkR_JASLUrU7y9eZkKDcBOykwNt3boMQYoEseRbznTkeH8Y-CzgSAPY4C0WnAGEKqAAK846tRGVcIcC592wFUqtCg_7zgX3M-QZAC63siuFVizy2Ybj-X1KIE6YuT13MfGz4tO2GPs59mLDm991AV_iLvOmwrzMfMCS-7aXQ8_U4D3VIHWYCp5b__H1ywTdjjf0e22lCn_HTU91lv76eXZ1-L84vv_04PTkvoqqqqUCs9LoyEC1a5UrQJljqOBGcdlpLIaWsjamhbFBLZctGSutqXcayFo40u-xgmXsfhoZ28jfjnAZy9O3jw9qjpP8BAUISebiQt2m8mzFPftPliH0fBhzn7IU12llHLKH7r9DnqdIJZ8App9-ihNWK9nO2IkosVExjzgkbf5u6TUiPXoDfBumXID091G-D9IY0ctFkYimn9GLyG6IvT0btOFzfke7ZyRhbQSmNU_8AVzWosA</recordid><startdate>2016</startdate><enddate>2016</enddate><creator>Zhang, Hongsheng</creator><creator>Zhao, Jiachen</creator><creator>Li, Penghui</creator><creator>Yue, Wenhan</creator><creator>Wang, Zhenxiang</creator><general>The Chinese Society of Oceanography</general><general>Springer Nature B.V</general><general>College of 0cean Science and Engineering, Shanghai Maritime University, Shanghai 201306, China%Yangtze River Estuary Investigation Bureau of Hydrology and Water Resource, Yangtze River Water Resource Commission, Shanghai 200136, China</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TG</scope><scope>7TN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</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>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>SOI</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>BBNVY</scope><scope>FR3</scope><scope>H95</scope><scope>H97</scope><scope>H98</scope><scope>H99</scope><scope>L.F</scope><scope>LK8</scope><scope>M7P</scope><scope>P64</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>2016</creationdate><title>The change characteristics of the calculated wind wave fields near lateral boundaries with SWAN model</title><author>Zhang, Hongsheng ; 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Sin</stitle><addtitle>Acta Oceanologica Sinica</addtitle><date>2016</date><risdate>2016</risdate><volume>35</volume><issue>1</issue><spage>96</spage><epage>105</epage><pages>96-105</pages><issn>0253-505X</issn><eissn>1869-1099</eissn><abstract>Since the wind wave model Simulating Waves Nearshore （SWAN） cannot effectively simulate the wave fields near the lateral boundaries, the change characteristics and the distortion ranges of calculated wave factors including wave heights, periods, directions, and lengths near the lateral boundaries of calculation domain are carefully studied in the case of different water depths and wind speeds respectively. The calculation results show that the effects of the variety of water depth and wind speed on the modeled different wave factors near the lateral boundaries are different. In the case of a certain wind speed, the greater the water depth is, the greater the distortion range is. In the case of a certain water depth, the distortion ranges defined by the relative errors of wave heights, periods, and lengths are different from those defined by the absolute errors of the corresponding wave factors. Moreover, the distortion ranges defined by the relative errors decrease with the increase of wind speed; whereas the distortion ranges defined by the absolute errors change a little with the variety of wind speed. The distortion range of wave direction decreases with the increase of wind speed. The calculated wave factors near the lateral boundaries with the SWAN model in the actual physical areas, such as Lake Taihu and Lake Dianshan considered in this study, are indeed distorted if the calculation domains are not enlarged on the basis of actual physical areas. Therefore, when SWAN is employed to calculate the wind wave fields near the shorelines of sea or inland lakes, the appropriate approaches must be adopted to reduce the calculation errors.</abstract><cop>Beijing</cop><pub>The Chinese Society of Oceanography</pub><doi>10.1007/s13131-016-0800-6</doi><tpages>10</tpages></addata></record> |
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| subjects | Boundaries Climatology Distortion Earth and Environmental Science Earth Sciences Ecology Engineering Fluid Dynamics Environmental Chemistry Errors Inland waters Lakes Marine Marine & Freshwater Sciences Oceanography Water depth Wave direction Wave height Wave power Wind Wind speed Wind waves 侧边界 天鹅 模型模拟 特征和 相对误差 绝对误差 计算域 风场 |
| title | The change characteristics of the calculated wind wave fields near lateral boundaries with SWAN model |
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