Evaluating the Accuracy of ERA5 Wave Reanalysis in the Water Around China
Wave parameters, such as wave height and wave period, are important for human activities, such as navigation, ocean engineering and sediment transport, etc. In this study, wave data from six buoys around Chinese waters, are used to assess the quality of wave height and wave period in the ERA5 reanal...
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description | Wave parameters, such as wave height and wave period, are important for human activities, such as navigation, ocean engineering and sediment transport,
etc.
In this study, wave data from six buoys around Chinese waters, are used to assess the quality of wave height and wave period in the ERA5 reanalysis of the European Centre for Medium-Range Weather Forecasts. Annual hourly data with temporal resolution are used. The difference between the significant wave height (SWH) of ERA 5 and that of the buoy varies from −0.35 m to 0.30 m for the three shallow locations; for the three deep locations, the variation ranges from −0.09 m to 0.09 m. The ERA5 SWH data show positive biases, indicating an overall overestimation for all locations, except for E2 and S1 where underestimation is observed. During the tropical cyclone period, a large (about 32%) underestimation of the maximum SWH in the ERA5 data is observed. Hence, the ERA5 SWH data cannot be used for design applications without site-specific validation. The difference between the annual wave period from ERA5 and the mean wave period from the buoys varies from −1.31s to 0.4s. Inter-comparisons suggest that the ERA5 dataset is consistent with the annual mean SWH. However, for the average period, the performance is not good, and half of the correlation coefficients in the four points are less 50%. Overall, the deep water area simulation effect is better than that in the shallow water. |
doi_str_mv | 10.1007/s11802-021-4496-7 |
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etc.
In this study, wave data from six buoys around Chinese waters, are used to assess the quality of wave height and wave period in the ERA5 reanalysis of the European Centre for Medium-Range Weather Forecasts. Annual hourly data with temporal resolution are used. The difference between the significant wave height (SWH) of ERA 5 and that of the buoy varies from −0.35 m to 0.30 m for the three shallow locations; for the three deep locations, the variation ranges from −0.09 m to 0.09 m. The ERA5 SWH data show positive biases, indicating an overall overestimation for all locations, except for E2 and S1 where underestimation is observed. During the tropical cyclone period, a large (about 32%) underestimation of the maximum SWH in the ERA5 data is observed. Hence, the ERA5 SWH data cannot be used for design applications without site-specific validation. The difference between the annual wave period from ERA5 and the mean wave period from the buoys varies from −1.31s to 0.4s. Inter-comparisons suggest that the ERA5 dataset is consistent with the annual mean SWH. However, for the average period, the performance is not good, and half of the correlation coefficients in the four points are less 50%. Overall, the deep water area simulation effect is better than that in the shallow water.</description><identifier>ISSN: 1672-5182</identifier><identifier>EISSN: 1993-5021</identifier><identifier>EISSN: 1672-5174</identifier><identifier>DOI: 10.1007/s11802-021-4496-7</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Body height ; Buoys ; Coefficients ; Correlation coefficient ; Correlation coefficients ; Cyclones ; Deep water ; Earth and Environmental Science ; Earth Sciences ; Hurricanes ; Locations (working) ; Meteorology ; Navigation ; Ocean engineering ; Oceanography ; Offshore engineering ; Quality assessment ; Sediment transport ; Shallow water ; Significant wave height ; Temporal resolution ; Tropical climate ; Tropical cyclones ; Wave data ; Wave height ; Wave parameters ; Wave period ; Weather forecasting</subject><ispartof>Journal of Ocean University of China, 2021-02, Vol.20 (1), p.1-9</ispartof><rights>Ocean University of China, Science Press and Springer-Verlag GmbH Germany 2021</rights><rights>Ocean University of China, Science Press and Springer-Verlag GmbH Germany 2021.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c418t-97a49a2ddf195a02e87a7dd2b59086e23ee6af346e21ac9445f71d7b051074693</citedby><cites>FETCH-LOGICAL-c418t-97a49a2ddf195a02e87a7dd2b59086e23ee6af346e21ac9445f71d7b051074693</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/qdhydxxb-e/qdhydxxb-e.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11802-021-4496-7$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11802-021-4496-7$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,41487,42556,51318</link.rule.ids></links><search><creatorcontrib>Shi, Hongyuan</creatorcontrib><creatorcontrib>Cao, Xuefeng</creatorcontrib><creatorcontrib>Li, Qingjie</creatorcontrib><creatorcontrib>Li, Delei</creatorcontrib><creatorcontrib>Sun, Jiacheng</creatorcontrib><creatorcontrib>You, Zaijin</creatorcontrib><creatorcontrib>Sun, Qingying</creatorcontrib><title>Evaluating the Accuracy of ERA5 Wave Reanalysis in the Water Around China</title><title>Journal of Ocean University of China</title><addtitle>J. Ocean Univ. China</addtitle><description>Wave parameters, such as wave height and wave period, are important for human activities, such as navigation, ocean engineering and sediment transport,
etc.
In this study, wave data from six buoys around Chinese waters, are used to assess the quality of wave height and wave period in the ERA5 reanalysis of the European Centre for Medium-Range Weather Forecasts. Annual hourly data with temporal resolution are used. The difference between the significant wave height (SWH) of ERA 5 and that of the buoy varies from −0.35 m to 0.30 m for the three shallow locations; for the three deep locations, the variation ranges from −0.09 m to 0.09 m. The ERA5 SWH data show positive biases, indicating an overall overestimation for all locations, except for E2 and S1 where underestimation is observed. During the tropical cyclone period, a large (about 32%) underestimation of the maximum SWH in the ERA5 data is observed. Hence, the ERA5 SWH data cannot be used for design applications without site-specific validation. The difference between the annual wave period from ERA5 and the mean wave period from the buoys varies from −1.31s to 0.4s. Inter-comparisons suggest that the ERA5 dataset is consistent with the annual mean SWH. However, for the average period, the performance is not good, and half of the correlation coefficients in the four points are less 50%. Overall, the deep water area simulation effect is better than that in the shallow water.</description><subject>Body height</subject><subject>Buoys</subject><subject>Coefficients</subject><subject>Correlation coefficient</subject><subject>Correlation coefficients</subject><subject>Cyclones</subject><subject>Deep water</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Hurricanes</subject><subject>Locations (working)</subject><subject>Meteorology</subject><subject>Navigation</subject><subject>Ocean engineering</subject><subject>Oceanography</subject><subject>Offshore engineering</subject><subject>Quality assessment</subject><subject>Sediment transport</subject><subject>Shallow water</subject><subject>Significant wave height</subject><subject>Temporal resolution</subject><subject>Tropical climate</subject><subject>Tropical cyclones</subject><subject>Wave data</subject><subject>Wave height</subject><subject>Wave parameters</subject><subject>Wave period</subject><subject>Weather forecasting</subject><issn>1672-5182</issn><issn>1993-5021</issn><issn>1672-5174</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp1kNFKwzAUhoMoOKcP4F3AS6kmadI0l2NMHQyEoewynDXp1jHTLWnn-vZmVtiVVzmE7_8550PonpInSoh8DpTmhCWE0YRzlSXyAg2oUmki4tdlnDPJEkFzdo1uQtgQIlKRyQGaTg6wbaGp3Ao3a4tHRdF6KDpcl3gyHwm8gIPFcwsOtl2oAq7cL7eAxno88nXrDB6vKwe36KqEbbB3f-8Qfb5MPsZvyez9dToezZKC07xJlASugBlTUiWAMJtLkMawpVAkzyxLrc2gTHkcKRSKc1FKauSSCEokz1Q6RI997ze4EtxKb-rWx-2C3pt1Z47HpbYsHk2iFxrph57e-Xrf2tCcccalZBmPYiJFe6rwdQjelnrnqy_wnaZEn_zq3q-OvfrkV8uYYX0mRNatrD83_x_6Ad5NetM</recordid><startdate>20210201</startdate><enddate>20210201</enddate><creator>Shi, Hongyuan</creator><creator>Cao, Xuefeng</creator><creator>Li, Qingjie</creator><creator>Li, Delei</creator><creator>Sun, Jiacheng</creator><creator>You, Zaijin</creator><creator>Sun, Qingying</creator><general>Science Press</general><general>Springer Nature B.V</general><general>Institute of Ports and Coastal Disaster Mitigation, Ludong University, Yantai 264025, China%National Marine Environmental Monitoring Center, Dalian 116023, China%Yantai Marine Environmental Monitoring Central Station, State Oceanic Administration, Yantai 264006, China%Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China%School of Civil Engineering, Ludong University, Yantai 264025, China</general><general>School of Civil Engineering, Ludong University, Yantai 264025, China</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7T7</scope><scope>7TN</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H95</scope><scope>H96</scope><scope>L.G</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>20210201</creationdate><title>Evaluating the Accuracy of ERA5 Wave Reanalysis in the Water Around China</title><author>Shi, Hongyuan ; Cao, Xuefeng ; Li, Qingjie ; Li, Delei ; Sun, Jiacheng ; You, Zaijin ; Sun, Qingying</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c418t-97a49a2ddf195a02e87a7dd2b59086e23ee6af346e21ac9445f71d7b051074693</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Body height</topic><topic>Buoys</topic><topic>Coefficients</topic><topic>Correlation coefficient</topic><topic>Correlation coefficients</topic><topic>Cyclones</topic><topic>Deep water</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Hurricanes</topic><topic>Locations (working)</topic><topic>Meteorology</topic><topic>Navigation</topic><topic>Ocean engineering</topic><topic>Oceanography</topic><topic>Offshore engineering</topic><topic>Quality assessment</topic><topic>Sediment transport</topic><topic>Shallow water</topic><topic>Significant wave height</topic><topic>Temporal resolution</topic><topic>Tropical climate</topic><topic>Tropical cyclones</topic><topic>Wave data</topic><topic>Wave height</topic><topic>Wave parameters</topic><topic>Wave period</topic><topic>Weather forecasting</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Shi, Hongyuan</creatorcontrib><creatorcontrib>Cao, Xuefeng</creatorcontrib><creatorcontrib>Li, Qingjie</creatorcontrib><creatorcontrib>Li, Delei</creatorcontrib><creatorcontrib>Sun, Jiacheng</creatorcontrib><creatorcontrib>You, Zaijin</creatorcontrib><creatorcontrib>Sun, Qingying</creatorcontrib><collection>CrossRef</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Oceanic Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Journal of Ocean University of China</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Shi, Hongyuan</au><au>Cao, Xuefeng</au><au>Li, Qingjie</au><au>Li, Delei</au><au>Sun, Jiacheng</au><au>You, Zaijin</au><au>Sun, Qingying</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Evaluating the Accuracy of ERA5 Wave Reanalysis in the Water Around China</atitle><jtitle>Journal of Ocean University of China</jtitle><stitle>J. Ocean Univ. China</stitle><date>2021-02-01</date><risdate>2021</risdate><volume>20</volume><issue>1</issue><spage>1</spage><epage>9</epage><pages>1-9</pages><issn>1672-5182</issn><eissn>1993-5021</eissn><eissn>1672-5174</eissn><abstract>Wave parameters, such as wave height and wave period, are important for human activities, such as navigation, ocean engineering and sediment transport,
etc.
In this study, wave data from six buoys around Chinese waters, are used to assess the quality of wave height and wave period in the ERA5 reanalysis of the European Centre for Medium-Range Weather Forecasts. Annual hourly data with temporal resolution are used. The difference between the significant wave height (SWH) of ERA 5 and that of the buoy varies from −0.35 m to 0.30 m for the three shallow locations; for the three deep locations, the variation ranges from −0.09 m to 0.09 m. The ERA5 SWH data show positive biases, indicating an overall overestimation for all locations, except for E2 and S1 where underestimation is observed. During the tropical cyclone period, a large (about 32%) underestimation of the maximum SWH in the ERA5 data is observed. Hence, the ERA5 SWH data cannot be used for design applications without site-specific validation. The difference between the annual wave period from ERA5 and the mean wave period from the buoys varies from −1.31s to 0.4s. Inter-comparisons suggest that the ERA5 dataset is consistent with the annual mean SWH. However, for the average period, the performance is not good, and half of the correlation coefficients in the four points are less 50%. Overall, the deep water area simulation effect is better than that in the shallow water.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s11802-021-4496-7</doi><tpages>9</tpages></addata></record> |
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subjects | Body height Buoys Coefficients Correlation coefficient Correlation coefficients Cyclones Deep water Earth and Environmental Science Earth Sciences Hurricanes Locations (working) Meteorology Navigation Ocean engineering Oceanography Offshore engineering Quality assessment Sediment transport Shallow water Significant wave height Temporal resolution Tropical climate Tropical cyclones Wave data Wave height Wave parameters Wave period Weather forecasting |
title | Evaluating the Accuracy of ERA5 Wave Reanalysis in the Water Around China |
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