Observation of interactions between internal tides and near-inertial waves after typhoon passage in the northern South China Sea
During the observational period of our study, Typhoon Hagupit passed over the mooring site and induced strong near-inertial waves (NIWs), which provided an opportunity to investigate the interactions between internal tides (ITs) and NIWs. Based on the mooring data, we compared the current spectra du...
Gespeichert in:
| Veröffentlicht in: | Chinese journal of oceanology and limnology 2015-09, Vol.33 (5), p.1279-1285 |
|---|---|
| Hauptverfasser: | , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 1285 |
|---|---|
| container_issue | 5 |
| container_start_page | 1279 |
| container_title | Chinese journal of oceanology and limnology |
| container_volume | 33 |
| creator | Lin, Feilong Liang, Chujin Hou, Yijun Liu, Yahao Liu, Ze Hu, Po |
| description | During the observational period of our study, Typhoon Hagupit passed over the mooring site and induced strong near-inertial waves (NIWs), which provided an opportunity to investigate the interactions between internal tides (ITs) and NIWs. Based on the mooring data, we compared the current spectra during the typhoon period and non-typhoon period in the northern South China Sea, and found that the high-frequency waves (fD₁ and fD₂) were evident during the former. Moreover, the observations of the current revealed that fD₁ and fD₂ occurred near the depth of strong vertical shear in the NIWs. In order to confirm the generation mechanism of fD₁ and fD₂, we compared the positions of strong vertical shear in the NIWs and strong vertical velocity in the ITs. It was established that the vertical shear of the horizontal current of the NIWs and the vertical current of the ITs contributed to the generation of fD₁ and fD₂. |
| doi_str_mv | 10.1007/s00343-015-4253-0 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_1709965693</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1722176438</sourcerecordid><originalsourceid>FETCH-LOGICAL-c373t-af5dfafc4ee34faa2e392bbbf54c854d119d265e87f6710b92778634056f0e6c3</originalsourceid><addsrcrecordid>eNp9kT9rHDEQxYWJwRc7HyBVBGnSrDP6t3sqwxEnBoOLi2sxuzu6W3OWLpLOxl0-erRsipAi1cw8fu_B8Bh7L-BaAHSfM4DSqgFhGi1NXc7YSlirGgNg3rAVSKMbDcZesLc5P1baarAr9uu-z5SesUwx8Oj5FAolHOYz857KC1FYxIAHXqaRMscw8kCYmilQKlPVX_B51n3FeHk97mMNO2LOuKNq5mVPPMRURwp8G09lzzf7KSDfEl6xc4-HTO_-zEv2cPP1x-Z7c3f_7Xbz5a4ZVKdKg96MHv2giZT2iJKUlX3fe6OHtdGjEHaUraF159tOQG9l161bVT9uPVA7qEv2ack9pvjzRLm4pykPdDhgoHjKTnRSiq7Val3Rj_-gj_E0_z9TYG1rWqsqJRZqSDHnRN4d0_SE6dUJcHMnbunE1U7c3ImD6pGLJ1c27Cj9lfwf04fF5DE63KUpu4etrACAFFIZqX4DaSaZqw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1709965693</pqid></control><display><type>article</type><title>Observation of interactions between internal tides and near-inertial waves after typhoon passage in the northern South China Sea</title><source>ProQuest Central Essentials</source><source>ProQuest Central (Alumni Edition)</source><source>ProQuest Central Student</source><source>Springer Nature - Complete Springer Journals</source><source>ProQuest Central Korea</source><source>ProQuest Central UK/Ireland</source><source>Alma/SFX Local Collection</source><source>ProQuest Central</source><creator>Lin, Feilong ; Liang, Chujin ; Hou, Yijun ; Liu, Yahao ; Liu, Ze ; Hu, Po</creator><creatorcontrib>Lin, Feilong ; Liang, Chujin ; Hou, Yijun ; Liu, Yahao ; Liu, Ze ; Hu, Po</creatorcontrib><description>During the observational period of our study, Typhoon Hagupit passed over the mooring site and induced strong near-inertial waves (NIWs), which provided an opportunity to investigate the interactions between internal tides (ITs) and NIWs. Based on the mooring data, we compared the current spectra during the typhoon period and non-typhoon period in the northern South China Sea, and found that the high-frequency waves (fD₁ and fD₂) were evident during the former. Moreover, the observations of the current revealed that fD₁ and fD₂ occurred near the depth of strong vertical shear in the NIWs. In order to confirm the generation mechanism of fD₁ and fD₂, we compared the positions of strong vertical shear in the NIWs and strong vertical velocity in the ITs. It was established that the vertical shear of the horizontal current of the NIWs and the vertical current of the ITs contributed to the generation of fD₁ and fD₂.</description><identifier>ISSN: 0254-4059</identifier><identifier>ISSN: 2096-5508</identifier><identifier>EISSN: 1993-5005</identifier><identifier>EISSN: 2523-3521</identifier><identifier>DOI: 10.1007/s00343-015-4253-0</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Current spectra ; Dynamics ; Earth and Environmental Science ; Earth Sciences ; Hurricanes ; Inertial waves ; Internal tides ; Marine ; Mooring ; Mooring systems ; Ocean waves ; Oceanography ; Physical oceanography ; Shear ; Tidal dynamics ; Tides ; Typhoons ; Vertical orientation ; Vertical shear ; Waves</subject><ispartof>Chinese journal of oceanology and limnology, 2015-09, Vol.33 (5), p.1279-1285</ispartof><rights>Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag Berlin Heidelberg 2015</rights><rights>Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag Berlin Heidelberg 2015.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c373t-af5dfafc4ee34faa2e392bbbf54c854d119d265e87f6710b92778634056f0e6c3</citedby><cites>FETCH-LOGICAL-c373t-af5dfafc4ee34faa2e392bbbf54c854d119d265e87f6710b92778634056f0e6c3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/1709965693/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/1709965693?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,776,780,21368,21369,21370,21371,23236,27903,27904,33509,33682,33723,33984,34293,43638,43766,43784,43932,44046,64362,64366,72216,73851,74030,74049,74220,74337</link.rule.ids></links><search><creatorcontrib>Lin, Feilong</creatorcontrib><creatorcontrib>Liang, Chujin</creatorcontrib><creatorcontrib>Hou, Yijun</creatorcontrib><creatorcontrib>Liu, Yahao</creatorcontrib><creatorcontrib>Liu, Ze</creatorcontrib><creatorcontrib>Hu, Po</creatorcontrib><title>Observation of interactions between internal tides and near-inertial waves after typhoon passage in the northern South China Sea</title><title>Chinese journal of oceanology and limnology</title><addtitle>Chin. J. Ocean. Limnol</addtitle><description>During the observational period of our study, Typhoon Hagupit passed over the mooring site and induced strong near-inertial waves (NIWs), which provided an opportunity to investigate the interactions between internal tides (ITs) and NIWs. Based on the mooring data, we compared the current spectra during the typhoon period and non-typhoon period in the northern South China Sea, and found that the high-frequency waves (fD₁ and fD₂) were evident during the former. Moreover, the observations of the current revealed that fD₁ and fD₂ occurred near the depth of strong vertical shear in the NIWs. In order to confirm the generation mechanism of fD₁ and fD₂, we compared the positions of strong vertical shear in the NIWs and strong vertical velocity in the ITs. It was established that the vertical shear of the horizontal current of the NIWs and the vertical current of the ITs contributed to the generation of fD₁ and fD₂.</description><subject>Current spectra</subject><subject>Dynamics</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Hurricanes</subject><subject>Inertial waves</subject><subject>Internal tides</subject><subject>Marine</subject><subject>Mooring</subject><subject>Mooring systems</subject><subject>Ocean waves</subject><subject>Oceanography</subject><subject>Physical oceanography</subject><subject>Shear</subject><subject>Tidal dynamics</subject><subject>Tides</subject><subject>Typhoons</subject><subject>Vertical orientation</subject><subject>Vertical shear</subject><subject>Waves</subject><issn>0254-4059</issn><issn>2096-5508</issn><issn>1993-5005</issn><issn>2523-3521</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kT9rHDEQxYWJwRc7HyBVBGnSrDP6t3sqwxEnBoOLi2sxuzu6W3OWLpLOxl0-erRsipAi1cw8fu_B8Bh7L-BaAHSfM4DSqgFhGi1NXc7YSlirGgNg3rAVSKMbDcZesLc5P1baarAr9uu-z5SesUwx8Oj5FAolHOYz857KC1FYxIAHXqaRMscw8kCYmilQKlPVX_B51n3FeHk97mMNO2LOuKNq5mVPPMRURwp8G09lzzf7KSDfEl6xc4-HTO_-zEv2cPP1x-Z7c3f_7Xbz5a4ZVKdKg96MHv2giZT2iJKUlX3fe6OHtdGjEHaUraF159tOQG9l161bVT9uPVA7qEv2ack9pvjzRLm4pykPdDhgoHjKTnRSiq7Val3Rj_-gj_E0_z9TYG1rWqsqJRZqSDHnRN4d0_SE6dUJcHMnbunE1U7c3ImD6pGLJ1c27Cj9lfwf04fF5DE63KUpu4etrACAFFIZqX4DaSaZqw</recordid><startdate>20150901</startdate><enddate>20150901</enddate><creator>Lin, Feilong</creator><creator>Liang, Chujin</creator><creator>Hou, Yijun</creator><creator>Liu, Yahao</creator><creator>Liu, Ze</creator><creator>Hu, Po</creator><general>Science Press</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7QL</scope><scope>7SN</scope><scope>7TN</scope><scope>7U7</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</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>L.G</scope><scope>M2P</scope><scope>M7N</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>7TG</scope><scope>8FD</scope><scope>FR3</scope><scope>H95</scope><scope>H99</scope><scope>KL.</scope><scope>L.F</scope><scope>P64</scope></search><sort><creationdate>20150901</creationdate><title>Observation of interactions between internal tides and near-inertial waves after typhoon passage in the northern South China Sea</title><author>Lin, Feilong ; Liang, Chujin ; Hou, Yijun ; Liu, Yahao ; Liu, Ze ; Hu, Po</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c373t-af5dfafc4ee34faa2e392bbbf54c854d119d265e87f6710b92778634056f0e6c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Current spectra</topic><topic>Dynamics</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Hurricanes</topic><topic>Inertial waves</topic><topic>Internal tides</topic><topic>Marine</topic><topic>Mooring</topic><topic>Mooring systems</topic><topic>Ocean waves</topic><topic>Oceanography</topic><topic>Physical oceanography</topic><topic>Shear</topic><topic>Tidal dynamics</topic><topic>Tides</topic><topic>Typhoons</topic><topic>Vertical orientation</topic><topic>Vertical shear</topic><topic>Waves</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lin, Feilong</creatorcontrib><creatorcontrib>Liang, Chujin</creatorcontrib><creatorcontrib>Hou, Yijun</creatorcontrib><creatorcontrib>Liu, Yahao</creatorcontrib><creatorcontrib>Liu, Ze</creatorcontrib><creatorcontrib>Hu, Po</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Aqualine</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Ecology Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Toxicology Abstracts</collection><collection>Water Resources 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>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</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 & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Earth, Atmospheric & 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>ProQuest Central Basic</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>ASFA: Marine Biotechnology Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Marine Biotechnology Abstracts</collection><collection>Biotechnology and BioEngineering Abstracts</collection><jtitle>Chinese journal of oceanology and limnology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lin, Feilong</au><au>Liang, Chujin</au><au>Hou, Yijun</au><au>Liu, Yahao</au><au>Liu, Ze</au><au>Hu, Po</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Observation of interactions between internal tides and near-inertial waves after typhoon passage in the northern South China Sea</atitle><jtitle>Chinese journal of oceanology and limnology</jtitle><stitle>Chin. J. Ocean. Limnol</stitle><date>2015-09-01</date><risdate>2015</risdate><volume>33</volume><issue>5</issue><spage>1279</spage><epage>1285</epage><pages>1279-1285</pages><issn>0254-4059</issn><issn>2096-5508</issn><eissn>1993-5005</eissn><eissn>2523-3521</eissn><abstract>During the observational period of our study, Typhoon Hagupit passed over the mooring site and induced strong near-inertial waves (NIWs), which provided an opportunity to investigate the interactions between internal tides (ITs) and NIWs. Based on the mooring data, we compared the current spectra during the typhoon period and non-typhoon period in the northern South China Sea, and found that the high-frequency waves (fD₁ and fD₂) were evident during the former. Moreover, the observations of the current revealed that fD₁ and fD₂ occurred near the depth of strong vertical shear in the NIWs. In order to confirm the generation mechanism of fD₁ and fD₂, we compared the positions of strong vertical shear in the NIWs and strong vertical velocity in the ITs. It was established that the vertical shear of the horizontal current of the NIWs and the vertical current of the ITs contributed to the generation of fD₁ and fD₂.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s00343-015-4253-0</doi><tpages>7</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0254-4059 |
| ispartof | Chinese journal of oceanology and limnology, 2015-09, Vol.33 (5), p.1279-1285 |
| issn | 0254-4059 2096-5508 1993-5005 2523-3521 |
| language | eng |
| recordid | cdi_proquest_journals_1709965693 |
| source | ProQuest Central Essentials; ProQuest Central (Alumni Edition); ProQuest Central Student; Springer Nature - Complete Springer Journals; ProQuest Central Korea; ProQuest Central UK/Ireland; Alma/SFX Local Collection; ProQuest Central |
| subjects | Current spectra Dynamics Earth and Environmental Science Earth Sciences Hurricanes Inertial waves Internal tides Marine Mooring Mooring systems Ocean waves Oceanography Physical oceanography Shear Tidal dynamics Tides Typhoons Vertical orientation Vertical shear Waves |
| title | Observation of interactions between internal tides and near-inertial waves after typhoon passage in the northern South China Sea |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-23T03%3A47%3A39IST&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=Observation%20of%20interactions%20between%20internal%20tides%20and%20near-inertial%20waves%20after%20typhoon%20passage%20in%20the%20northern%20South%20China%20Sea&rft.jtitle=Chinese%20journal%20of%20oceanology%20and%20limnology&rft.au=Lin,%20Feilong&rft.date=2015-09-01&rft.volume=33&rft.issue=5&rft.spage=1279&rft.epage=1285&rft.pages=1279-1285&rft.issn=0254-4059&rft.eissn=1993-5005&rft_id=info:doi/10.1007/s00343-015-4253-0&rft_dat=%3Cproquest_cross%3E1722176438%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=1709965693&rft_id=info:pmid/&rfr_iscdi=true |