Has wind–wave modeling reached its limit?
This article uses a comparison of four different numerical wave prediction models for hindcast wave conditions in Lake Michigan during a 10-day episode in October 1988 to illustrate that typical wave prediction models based on the concept of a wave energy spectrum may have reached a limit in the acc...
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Veröffentlicht in: | Ocean engineering 2002-01, Vol.29 (1), p.81-98 |
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description | This article uses a comparison of four different numerical wave prediction models for hindcast wave conditions in Lake Michigan during a 10-day episode in October 1988 to illustrate that typical wave prediction models based on the concept of a wave energy spectrum may have reached a limit in the accuracy with which they can simulate realistic wave generation and growth conditions. In the hindcast study we compared the model results to observed wave height and period measurements from two deep water NOAA/NDBC weather buoys and from a nearshore Waverider buoy. Hourly wind fields interpolated from a large number of coastal and overlake observations were used to drive the models. The same numerical grid was used for all the models. The results show that while the individual model predictions deviate from the measurements by various amounts, they all tend to reflect the general trend and patterns of the wave measurements. The differences between the model results are often similar in magnitude to differences between model results and observations. Although the four models tested represent a wide range of sophistication in their treatment of wave growth dynamics, they are all based on the assumption that the sea state can be represented by a wave energy spectrum. Because there are more similarities among the model results than significant differences, we believe that this assumption may be the limiting factor for substantial improvements in wave modeling. |
doi_str_mv | 10.1016/S0029-8018(00)00074-3 |
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In the hindcast study we compared the model results to observed wave height and period measurements from two deep water NOAA/NDBC weather buoys and from a nearshore Waverider buoy. Hourly wind fields interpolated from a large number of coastal and overlake observations were used to drive the models. The same numerical grid was used for all the models. The results show that while the individual model predictions deviate from the measurements by various amounts, they all tend to reflect the general trend and patterns of the wave measurements. The differences between the model results are often similar in magnitude to differences between model results and observations. Although the four models tested represent a wide range of sophistication in their treatment of wave growth dynamics, they are all based on the assumption that the sea state can be represented by a wave energy spectrum. Because there are more similarities among the model results than significant differences, we believe that this assumption may be the limiting factor for substantial improvements in wave modeling.</description><identifier>ISSN: 0029-8018</identifier><identifier>EISSN: 1873-5258</identifier><identifier>DOI: 10.1016/S0029-8018(00)00074-3</identifier><identifier>CODEN: OCENBQ</identifier><language>eng</language><publisher>Amsterdam: Elsevier Ltd</publisher><subject>Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Freshwater ; Ocean waves ; Physics of the oceans ; Sea-air exchange processes ; WAM model ; Wave modeling ; Wind waves</subject><ispartof>Ocean engineering, 2002-01, Vol.29 (1), p.81-98</ispartof><rights>2001</rights><rights>2002 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c368t-3d1b2331c91b4cb47c83556b22c92bd26a795a1a52f7198c9e55a40bf6d739a53</citedby><cites>FETCH-LOGICAL-c368t-3d1b2331c91b4cb47c83556b22c92bd26a795a1a52f7198c9e55a40bf6d739a53</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0029801800000743$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3536,27903,27904,65309</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=13398726$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Liu, Paul C.</creatorcontrib><creatorcontrib>Schwab, David J.</creatorcontrib><creatorcontrib>Jensen, Robert E.</creatorcontrib><title>Has wind–wave modeling reached its limit?</title><title>Ocean engineering</title><description>This article uses a comparison of four different numerical wave prediction models for hindcast wave conditions in Lake Michigan during a 10-day episode in October 1988 to illustrate that typical wave prediction models based on the concept of a wave energy spectrum may have reached a limit in the accuracy with which they can simulate realistic wave generation and growth conditions. In the hindcast study we compared the model results to observed wave height and period measurements from two deep water NOAA/NDBC weather buoys and from a nearshore Waverider buoy. Hourly wind fields interpolated from a large number of coastal and overlake observations were used to drive the models. The same numerical grid was used for all the models. The results show that while the individual model predictions deviate from the measurements by various amounts, they all tend to reflect the general trend and patterns of the wave measurements. The differences between the model results are often similar in magnitude to differences between model results and observations. Although the four models tested represent a wide range of sophistication in their treatment of wave growth dynamics, they are all based on the assumption that the sea state can be represented by a wave energy spectrum. Because there are more similarities among the model results than significant differences, we believe that this assumption may be the limiting factor for substantial improvements in wave modeling.</description><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Freshwater</subject><subject>Ocean waves</subject><subject>Physics of the oceans</subject><subject>Sea-air exchange processes</subject><subject>WAM model</subject><subject>Wave modeling</subject><subject>Wind waves</subject><issn>0029-8018</issn><issn>1873-5258</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><recordid>eNqFkM1KAzEcxIMoWKuPIOxFUWT1n2STTU5Filqh4EE9h2yS1ch-1GTb4s138A19Ercf6NHTXH4zwwxCxxguMWB-9QhAZCoAizOAcwDIs5TuoAEWOU0ZYWIXDX6RfXQQ41sPcQ50gC4mOiZL39jvz6-lXrikbq2rfPOSBKfNq7OJ72JS-dp3o0O0V-oquqOtDtHz7c3TeJJOH-7ux9fT1FAuupRaXBBKsZG4yEyR5UZQxnhBiJGksITrXDKNNSNljqUw0jGmMyhKbnMqNaNDdLrJnYX2fe5ip2ofjasq3bh2HhUWNOOS8h5kG9CENsbgSjULvtbhQ2FQq2vU-hq12q0A1PoaRXvfybZAR6OrMujG-PhnplSKnKzyRxvO9WsX3gUVjXeNcdYHZzplW_9P0w_a53bO</recordid><startdate>20020101</startdate><enddate>20020101</enddate><creator>Liu, Paul C.</creator><creator>Schwab, David J.</creator><creator>Jensen, Robert E.</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20020101</creationdate><title>Has wind–wave modeling reached its limit?</title><author>Liu, Paul C. ; Schwab, David J. ; Jensen, Robert E.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c368t-3d1b2331c91b4cb47c83556b22c92bd26a795a1a52f7198c9e55a40bf6d739a53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2002</creationdate><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Freshwater</topic><topic>Ocean waves</topic><topic>Physics of the oceans</topic><topic>Sea-air exchange processes</topic><topic>WAM model</topic><topic>Wave modeling</topic><topic>Wind waves</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liu, Paul C.</creatorcontrib><creatorcontrib>Schwab, David J.</creatorcontrib><creatorcontrib>Jensen, Robert E.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Ocean engineering</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liu, Paul C.</au><au>Schwab, David J.</au><au>Jensen, Robert E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Has wind–wave modeling reached its limit?</atitle><jtitle>Ocean engineering</jtitle><date>2002-01-01</date><risdate>2002</risdate><volume>29</volume><issue>1</issue><spage>81</spage><epage>98</epage><pages>81-98</pages><issn>0029-8018</issn><eissn>1873-5258</eissn><coden>OCENBQ</coden><abstract>This article uses a comparison of four different numerical wave prediction models for hindcast wave conditions in Lake Michigan during a 10-day episode in October 1988 to illustrate that typical wave prediction models based on the concept of a wave energy spectrum may have reached a limit in the accuracy with which they can simulate realistic wave generation and growth conditions. In the hindcast study we compared the model results to observed wave height and period measurements from two deep water NOAA/NDBC weather buoys and from a nearshore Waverider buoy. Hourly wind fields interpolated from a large number of coastal and overlake observations were used to drive the models. The same numerical grid was used for all the models. The results show that while the individual model predictions deviate from the measurements by various amounts, they all tend to reflect the general trend and patterns of the wave measurements. The differences between the model results are often similar in magnitude to differences between model results and observations. Although the four models tested represent a wide range of sophistication in their treatment of wave growth dynamics, they are all based on the assumption that the sea state can be represented by a wave energy spectrum. Because there are more similarities among the model results than significant differences, we believe that this assumption may be the limiting factor for substantial improvements in wave modeling.</abstract><cop>Amsterdam</cop><pub>Elsevier Ltd</pub><doi>10.1016/S0029-8018(00)00074-3</doi><tpages>18</tpages></addata></record> |
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subjects | Earth, ocean, space Exact sciences and technology External geophysics Freshwater Ocean waves Physics of the oceans Sea-air exchange processes WAM model Wave modeling Wind waves |
title | Has wind–wave modeling reached its limit? |
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