Estimates of global M2 internal tide energy fluxes using TOPEX/POSEIDON altimeter data
TOPEX/POSEIDON altimeter data from October 1992 to June 2002 are used to calculate the global barotropic M2 tidal currents using long-term tidal harmonic analysis. The tides calculated agree well with ADCP data obtained from the South China Sea （SCS）. The maximum tide velocities along the semi-major...
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| Veröffentlicht in: | Chinese journal of oceanology and limnology 2009-02, Vol.27 (1), p.129-134 |
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| description | TOPEX/POSEIDON altimeter data from October 1992 to June 2002 are used to calculate the global barotropic M2 tidal currents using long-term tidal harmonic analysis. The tides calculated agree well with ADCP data obtained from the South China Sea （SCS）. The maximum tide velocities along the semi-major axis and semi-minor axis can be computed from the tidal ellipse. The global distribution of M2 internal tide vertical energy flux from the sea bottom is calculated based on a linear internal wave generation model. The global vertical energy flux of M2 internal tide is 0.96 TW, with 0.36 TW in the Pacific, 0.31 TW in the Atlantic and 0.29 TW in the Indian Ocean, obtained in this study. The total horizontal energy flux of M2 internal tide radiating into the open ocean from the lateral boundaries is 0.13 TW, with 0.06 TW in the Pacific, 0.04TW in the Atlantic, and 0.03 TW in the Indian Ocean. The result shows that the principal lunar semi-diurnal tide Me provides enough energy to maintain the large-scale thermohaline circulation of the ocean. |
| doi_str_mv | 10.1007/s00343-009-0129-5 |
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The tides calculated agree well with ADCP data obtained from the South China Sea （SCS）. The maximum tide velocities along the semi-major axis and semi-minor axis can be computed from the tidal ellipse. The global distribution of M2 internal tide vertical energy flux from the sea bottom is calculated based on a linear internal wave generation model. The global vertical energy flux of M2 internal tide is 0.96 TW, with 0.36 TW in the Pacific, 0.31 TW in the Atlantic and 0.29 TW in the Indian Ocean, obtained in this study. The total horizontal energy flux of M2 internal tide radiating into the open ocean from the lateral boundaries is 0.13 TW, with 0.06 TW in the Pacific, 0.04TW in the Atlantic, and 0.03 TW in the Indian Ocean. The result shows that the principal lunar semi-diurnal tide Me provides enough energy to maintain the large-scale thermohaline circulation of the ocean.</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/s00343-009-0129-5</identifier><language>eng</language><publisher>Heidelberg: SP Science Press</publisher><subject>ADCP ; Altimeters ; Altimetry ; Barotropic mode ; Diurnal tides ; Earth and Environmental Science ; Earth Sciences ; Energy ; Energy transfer ; Fluctuations ; Fourier analysis ; Harmonic analysis ; Internal tides ; Internal wave generation ; Internal waves ; Oceanography ; Thermohaline circulation ; Tidal analysis ; Tidal currents ; Tidal energy ; TOPEX ; TOPEX卫星 ; Wave generation ; 测高数据 ; 能量通量 ; 调和分析</subject><ispartof>Chinese journal of oceanology and limnology, 2009-02, Vol.27 (1), p.129-134</ispartof><rights>Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag Berlin Heidelberg 2009</rights><rights>Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag Berlin Heidelberg 2009.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c1322-60a60bd21098613852488c29898f3704e58fe7a87a283dc717b0a7cac03f93f83</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/84119X/84119X.jpg</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2918064312/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2918064312?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,780,784,21388,21389,21390,21391,23256,27924,27925,33530,33703,33744,34005,34314,43659,43787,43805,43953,44067,64385,64389,72469,74104,74283,74302,74473,74590</link.rule.ids></links><search><creatorcontrib>张艳伟 梁鑫峰 田纪伟 杨丽芬</creatorcontrib><title>Estimates of global M2 internal tide energy fluxes using TOPEX/POSEIDON altimeter data</title><title>Chinese journal of oceanology and limnology</title><addtitle>Chin. J. Ocean. Limnol</addtitle><addtitle>Chinese Journal of Oceanology and Limnology</addtitle><description>TOPEX/POSEIDON altimeter data from October 1992 to June 2002 are used to calculate the global barotropic M2 tidal currents using long-term tidal harmonic analysis. The tides calculated agree well with ADCP data obtained from the South China Sea （SCS）. The maximum tide velocities along the semi-major axis and semi-minor axis can be computed from the tidal ellipse. The global distribution of M2 internal tide vertical energy flux from the sea bottom is calculated based on a linear internal wave generation model. The global vertical energy flux of M2 internal tide is 0.96 TW, with 0.36 TW in the Pacific, 0.31 TW in the Atlantic and 0.29 TW in the Indian Ocean, obtained in this study. The total horizontal energy flux of M2 internal tide radiating into the open ocean from the lateral boundaries is 0.13 TW, with 0.06 TW in the Pacific, 0.04TW in the Atlantic, and 0.03 TW in the Indian Ocean. The result shows that the principal lunar semi-diurnal tide Me provides enough energy to maintain the large-scale thermohaline circulation of the ocean.</description><subject>ADCP</subject><subject>Altimeters</subject><subject>Altimetry</subject><subject>Barotropic mode</subject><subject>Diurnal tides</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Energy</subject><subject>Energy transfer</subject><subject>Fluctuations</subject><subject>Fourier analysis</subject><subject>Harmonic analysis</subject><subject>Internal tides</subject><subject>Internal wave generation</subject><subject>Internal waves</subject><subject>Oceanography</subject><subject>Thermohaline circulation</subject><subject>Tidal analysis</subject><subject>Tidal currents</subject><subject>Tidal energy</subject><subject>TOPEX</subject><subject>TOPEX卫星</subject><subject>Wave generation</subject><subject>测高数据</subject><subject>能量通量</subject><subject>调和分析</subject><issn>0254-4059</issn><issn>2096-5508</issn><issn>1993-5005</issn><issn>2523-3521</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</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>eNpFkUFPwjAYhhujiYj-AG-NnjxMvrbr1h4NopKgkIjGW9Nt7RjODdYRgV9vyUw49Ts875uvz4fQNYF7AhAPHAALWQAgAyBUBvwE9YiULOAA_BT1gPIwCIHLc3Th3NLTMgTZQ58j1xY_ujUO1xbnZZ3oEr9SXFStaSo_t0VmsKlMk--wLTdbD25cUeV4Pp2Nvgaz6fto_Dh9w7r0PcaHcKZbfYnOrC6dufp_--jjaTQfvgST6fN4-DAJUsIoDSLQESQZJSBFRJjgNBQipVJIYVkMoeHCmliLWFPBsjQmcQI6TnUKzEpmBeuju673V1dWV7la1pvD2k7t88Vusd8m1CsBApR69rZjV0293hjXHmEqiYAoZORA0Y5yq8Z_0zRHioA6uFada-WL1cG14j5004XSRV3la59TiU6_bVEaxcBfgDDO_gA9KnoG</recordid><startdate>20090201</startdate><enddate>20090201</enddate><creator>张艳伟 梁鑫峰 田纪伟 杨丽芬</creator><general>SP Science Press</general><general>Springer Nature B.V</general><general>Physical Oceanography Laboratory, Ocean University of China, Qingdao 266100, 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杨丽芬</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c1322-60a60bd21098613852488c29898f3704e58fe7a87a283dc717b0a7cac03f93f83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>ADCP</topic><topic>Altimeters</topic><topic>Altimetry</topic><topic>Barotropic mode</topic><topic>Diurnal tides</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Energy</topic><topic>Energy transfer</topic><topic>Fluctuations</topic><topic>Fourier analysis</topic><topic>Harmonic analysis</topic><topic>Internal tides</topic><topic>Internal wave generation</topic><topic>Internal waves</topic><topic>Oceanography</topic><topic>Thermohaline circulation</topic><topic>Tidal analysis</topic><topic>Tidal currents</topic><topic>Tidal energy</topic><topic>TOPEX</topic><topic>TOPEX卫星</topic><topic>Wave 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J. Ocean. Limnol</stitle><addtitle>Chinese Journal of Oceanology and Limnology</addtitle><date>2009-02-01</date><risdate>2009</risdate><volume>27</volume><issue>1</issue><spage>129</spage><epage>134</epage><pages>129-134</pages><issn>0254-4059</issn><issn>2096-5508</issn><eissn>1993-5005</eissn><eissn>2523-3521</eissn><abstract>TOPEX/POSEIDON altimeter data from October 1992 to June 2002 are used to calculate the global barotropic M2 tidal currents using long-term tidal harmonic analysis. The tides calculated agree well with ADCP data obtained from the South China Sea （SCS）. The maximum tide velocities along the semi-major axis and semi-minor axis can be computed from the tidal ellipse. The global distribution of M2 internal tide vertical energy flux from the sea bottom is calculated based on a linear internal wave generation model. The global vertical energy flux of M2 internal tide is 0.96 TW, with 0.36 TW in the Pacific, 0.31 TW in the Atlantic and 0.29 TW in the Indian Ocean, obtained in this study. The total horizontal energy flux of M2 internal tide radiating into the open ocean from the lateral boundaries is 0.13 TW, with 0.06 TW in the Pacific, 0.04TW in the Atlantic, and 0.03 TW in the Indian Ocean. The result shows that the principal lunar semi-diurnal tide Me provides enough energy to maintain the large-scale thermohaline circulation of the ocean.</abstract><cop>Heidelberg</cop><pub>SP Science Press</pub><doi>10.1007/s00343-009-0129-5</doi><tpages>6</tpages></addata></record> |
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| subjects | ADCP Altimeters Altimetry Barotropic mode Diurnal tides Earth and Environmental Science Earth Sciences Energy Energy transfer Fluctuations Fourier analysis Harmonic analysis Internal tides Internal wave generation Internal waves Oceanography Thermohaline circulation Tidal analysis Tidal currents Tidal energy TOPEX TOPEX卫星 Wave generation 测高数据 能量通量 调和分析 |
| title | Estimates of global M2 internal tide energy fluxes using TOPEX/POSEIDON altimeter data |
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