Contribution of Mesoscale Eddies to the Subduction and Transport of North Pacific Eastern Subtropical Mode Water
This study investigates the contribution of mesoscale eddies to the subduction and transport of North Pacific Eastern Subtropical Mode Water (ESTMW) using the high-frequency output of an eddy-resolved ocean model spanning the period 1994–2010. Results show that the subduction induced by mesoscale ed...
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Veröffentlicht in: | Journal of Ocean University of China 2020-02, Vol.19 (1), p.36-46 |
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description | This study investigates the contribution of mesoscale eddies to the subduction and transport of North Pacific Eastern Subtropical Mode Water (ESTMW) using the high-frequency output of an eddy-resolved ocean model spanning the period 1994–2010. Results show that the subduction induced by mesoscale eddies accounts for about 31% of the total subduction of ESTMW formation. The volume of ESTMW trapped by anticyclonic eddies is slightly larger than that trapped by cyclonic eddies. The ESTMW trapped by all eddies in May reaches up to about 2.8 × 1013 m3, which is approximately 16% of the total ESTMW volume. The eddy-trapped ESTMW moves primarily westward, with its meridional integration at 18°–30°N reaching about 0.17 Sv, which is approximately 18% of the total zonal ESTMW transport in this direction, at 140°W. This study highlights the important role of eddies in carrying ESTMW westward over the northeastern Pacific Ocean. |
doi_str_mv | 10.1007/s11802-020-4203-0 |
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Results show that the subduction induced by mesoscale eddies accounts for about 31% of the total subduction of ESTMW formation. The volume of ESTMW trapped by anticyclonic eddies is slightly larger than that trapped by cyclonic eddies. The ESTMW trapped by all eddies in May reaches up to about 2.8 × 1013 m3, which is approximately 16% of the total ESTMW volume. The eddy-trapped ESTMW moves primarily westward, with its meridional integration at 18°–30°N reaching about 0.17 Sv, which is approximately 18% of the total zonal ESTMW transport in this direction, at 140°W. This study highlights the important role of eddies in carrying ESTMW westward over the northeastern Pacific Ocean.</description><identifier>ISSN: 1672-5182</identifier><identifier>EISSN: 1993-5021</identifier><identifier>EISSN: 1672-5174</identifier><identifier>DOI: 10.1007/s11802-020-4203-0</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Current rings ; Earth and Environmental Science ; Earth Sciences ; Eddies ; Mesoscale eddies ; Mesoscale phenomena ; Meteorology ; Ocean circulation ; Ocean models ; Oceanography ; Subduction ; Transport ; Vortices</subject><ispartof>Journal of Ocean University of China, 2020-02, Vol.19 (1), p.36-46</ispartof><rights>Ocean University of China, Science Press and Springer-Verlag GmbH Germany 2019</rights><rights>2019© Ocean University of China, Science Press and Springer-Verlag GmbH Germany 2019</rights><rights>Copyright © Wanfang Data Co. Ltd. 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Ocean Univ. China</addtitle><description>This study investigates the contribution of mesoscale eddies to the subduction and transport of North Pacific Eastern Subtropical Mode Water (ESTMW) using the high-frequency output of an eddy-resolved ocean model spanning the period 1994–2010. Results show that the subduction induced by mesoscale eddies accounts for about 31% of the total subduction of ESTMW formation. The volume of ESTMW trapped by anticyclonic eddies is slightly larger than that trapped by cyclonic eddies. The ESTMW trapped by all eddies in May reaches up to about 2.8 × 1013 m3, which is approximately 16% of the total ESTMW volume. The eddy-trapped ESTMW moves primarily westward, with its meridional integration at 18°–30°N reaching about 0.17 Sv, which is approximately 18% of the total zonal ESTMW transport in this direction, at 140°W. This study highlights the important role of eddies in carrying ESTMW westward over the northeastern Pacific Ocean.</description><subject>Current rings</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Eddies</subject><subject>Mesoscale eddies</subject><subject>Mesoscale phenomena</subject><subject>Meteorology</subject><subject>Ocean circulation</subject><subject>Ocean models</subject><subject>Oceanography</subject><subject>Subduction</subject><subject>Transport</subject><subject>Vortices</subject><issn>1672-5182</issn><issn>1993-5021</issn><issn>1672-5174</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp1kU1LxDAQhosoqKs_wFvAo1Tz0bTboyzrB-yq4IrHMG0mbkWTmqSo_96sFfbkaYbwPG9g3iw7YfScUVpdBMamlOeU07zgVOR0JztgdS1ySTnbTXtZ8VyyKd_PDkN4pVQKWVYHWT9zNvquGWLnLHGGLDG40MIbkrnWHQYSHYlrJI9Do4f2lwKrycqDDb3zcePcpbkmD9B2pmvJHEJEbzdG9K7vUhhZOo3kGdL7UbZn4C3g8d-cZE9X89XsJl_cX9_OLhd5KySPed2UDKuyKo2R7RRrUyDUhhagJXDQwAVHihoaAW2dUORaV6KsmWm0bpCJSXY25n6CNWBf1KsbvE0_qg-9_tZfX41Cns5F0_mKRJ-OdO_dx4AhbnEuCsGnQtYiUWykWu9C8GhU77t38N-KUbWpQY01qJSrNjUomhw-OiGx9gX9Nvl_6QeQ5ow5</recordid><startdate>20200201</startdate><enddate>20200201</enddate><creator>Yang, Zhitong</creator><creator>Luo, Yiyong</creator><general>Science Press</general><general>Springer Nature B.V</general><general>Physical Oceanography Laboratory/CIMST,Ocean University of China and Qingdao National Laboratory for Marine Science and Technology,Qingdao 266100,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>20200201</creationdate><title>Contribution of Mesoscale Eddies to the Subduction and Transport of North Pacific Eastern Subtropical Mode Water</title><author>Yang, Zhitong ; Luo, Yiyong</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c352t-9b61e7676ff5c8e9f4ea9f04ad5a2ada232e0edab3ac961ee2dd73691fbddbe13</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Current rings</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Eddies</topic><topic>Mesoscale eddies</topic><topic>Mesoscale phenomena</topic><topic>Meteorology</topic><topic>Ocean circulation</topic><topic>Ocean models</topic><topic>Oceanography</topic><topic>Subduction</topic><topic>Transport</topic><topic>Vortices</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Yang, Zhitong</creatorcontrib><creatorcontrib>Luo, Yiyong</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>Yang, Zhitong</au><au>Luo, Yiyong</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Contribution of Mesoscale Eddies to the Subduction and Transport of North Pacific Eastern Subtropical Mode Water</atitle><jtitle>Journal of Ocean University of China</jtitle><stitle>J. Ocean Univ. China</stitle><date>2020-02-01</date><risdate>2020</risdate><volume>19</volume><issue>1</issue><spage>36</spage><epage>46</epage><pages>36-46</pages><issn>1672-5182</issn><eissn>1993-5021</eissn><eissn>1672-5174</eissn><abstract>This study investigates the contribution of mesoscale eddies to the subduction and transport of North Pacific Eastern Subtropical Mode Water (ESTMW) using the high-frequency output of an eddy-resolved ocean model spanning the period 1994–2010. Results show that the subduction induced by mesoscale eddies accounts for about 31% of the total subduction of ESTMW formation. The volume of ESTMW trapped by anticyclonic eddies is slightly larger than that trapped by cyclonic eddies. The ESTMW trapped by all eddies in May reaches up to about 2.8 × 1013 m3, which is approximately 16% of the total ESTMW volume. The eddy-trapped ESTMW moves primarily westward, with its meridional integration at 18°–30°N reaching about 0.17 Sv, which is approximately 18% of the total zonal ESTMW transport in this direction, at 140°W. This study highlights the important role of eddies in carrying ESTMW westward over the northeastern Pacific Ocean.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s11802-020-4203-0</doi><tpages>11</tpages></addata></record> |
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subjects | Current rings Earth and Environmental Science Earth Sciences Eddies Mesoscale eddies Mesoscale phenomena Meteorology Ocean circulation Ocean models Oceanography Subduction Transport Vortices |
title | Contribution of Mesoscale Eddies to the Subduction and Transport of North Pacific Eastern Subtropical Mode Water |
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