Winter Meso-Scale Shear Front in the Yellow Sea and Its Sedimentary Effects
In this paper, the authors explored the presence of shear fronts between the Yellow Sea Coastal Current （YSCC） and the monsoon-strengthened Yellow Sea Warm Current （YSWC） in winter and their sedimentary effects within the shear zone based on a fully validated numerical model. This work added the win...
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| Veröffentlicht in: | Journal of Ocean University of China 2016-02, Vol.15 (1), p.50-56 |
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| description | In this paper, the authors explored the presence of shear fronts between the Yellow Sea Coastal Current （YSCC） and the monsoon-strengthened Yellow Sea Warm Current （YSWC） in winter and their sedimentary effects within the shear zone based on a fully validated numerical model. This work added the wind force to a tidal model during simulating the winter baroclinic circulation in the Yellow Sea. The results indicate that the YSWC is significantly strengthened by wind-driven compensation due to a northeast monsoon during winter time. When this warm current encounters the North Shandong-South Yellow Sea coastal current, there is a strong reverse shear action between the two current systems, forming a reverse-S-shaped shear front that begins near 34°N in the south and extends to approximately 38°N, with an overall length of over 600km. The main driving force for the formation of this shear front derives from the circulation system with the reverse flow. In the shear zone, temperature and salinity gradients increase, flow velocities are relatively small and the flow direction on one side of the shear zone is opposite to that on the other side. The ver- tical circulation structure is complicated, consisting of a series ofmeso- and small-scale anti-clockwise eddies. Particularly, this shear effect significantly hinders the horizontal exchange of coastal sediments carried by warm currents, resulting in fine sediments deposi- tion due to the weak hydrodynamic regime. |
| doi_str_mv | 10.1007/s11802-016-2668-7 |
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| fullrecord | <record><control><sourceid>wanfang_jour_proqu</sourceid><recordid>TN_cdi_wanfang_journals_qdhydxxb_e201601007</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cqvip_id>668040135</cqvip_id><wanfj_id>qdhydxxb_e201601007</wanfj_id><sourcerecordid>qdhydxxb_e201601007</sourcerecordid><originalsourceid>FETCH-LOGICAL-c412t-25b4211b1445cceefbcac14b9b15eae67f9a6c7dcdb7b6ccd83d7a3114b7fb4d3</originalsourceid><addsrcrecordid>eNp9kUtPHDEQhEcoSDySH5CbBRekyInbz50jQpCgEHFYUJST5UfP7qBdD2vPCvj38WoQQjnk5D58VdWubprPwL4CY-ZbAZgxThloyrWeUbPXHELbCqoYhw911oZTBTN-0ByV8sCYEkqbw-bn7z6NmMkvLAOdB7dCMl-iy-QqD2kkfSLjEskfXK2GJzJHR1yK5HosdY79GtPo8gu57DoMY_nY7HduVfDT63vc3F9d3l38oDe3368vzm9okMBHypWXHMCDlCoExM4HF0D61oNCh9p0rdPBxBC98TqEOBPROAEVMZ2XURw3XybfJ5c6lxb2YdjmVBPtJi5f4vOzt8hrE2zXTKXPJvoxD5stltGu-xLqh1zCYVssGK1ao5QUFT39B31zBqM0E8pwWSmYqJCHUjJ29jH369qDBWZ3kXY6hq0r2N0x7G4JPmlKZdMC8zvn_4hOXoOWQ1psqu4tqQJMMhBK_AXEXJbY</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1756035724</pqid></control><display><type>article</type><title>Winter Meso-Scale Shear Front in the Yellow Sea and Its Sedimentary Effects</title><source>Springer Nature - Complete Springer Journals</source><source>Alma/SFX Local Collection</source><creator>Gao, Fei ; Qiao, Lulu ; Li, Guangxue</creator><creatorcontrib>Gao, Fei ; Qiao, Lulu ; Li, Guangxue</creatorcontrib><description>In this paper, the authors explored the presence of shear fronts between the Yellow Sea Coastal Current （YSCC） and the monsoon-strengthened Yellow Sea Warm Current （YSWC） in winter and their sedimentary effects within the shear zone based on a fully validated numerical model. This work added the wind force to a tidal model during simulating the winter baroclinic circulation in the Yellow Sea. The results indicate that the YSWC is significantly strengthened by wind-driven compensation due to a northeast monsoon during winter time. When this warm current encounters the North Shandong-South Yellow Sea coastal current, there is a strong reverse shear action between the two current systems, forming a reverse-S-shaped shear front that begins near 34°N in the south and extends to approximately 38°N, with an overall length of over 600km. The main driving force for the formation of this shear front derives from the circulation system with the reverse flow. In the shear zone, temperature and salinity gradients increase, flow velocities are relatively small and the flow direction on one side of the shear zone is opposite to that on the other side. The ver- tical circulation structure is complicated, consisting of a series ofmeso- and small-scale anti-clockwise eddies. Particularly, this shear effect significantly hinders the horizontal exchange of coastal sediments carried by warm currents, resulting in fine sediments deposi- tion due to the weak hydrodynamic regime.</description><identifier>ISSN: 1672-5182</identifier><identifier>EISSN: 1993-5021</identifier><identifier>EISSN: 1672-5174</identifier><identifier>DOI: 10.1007/s11802-016-2668-7</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Coastal currents ; Earth and Environmental Science ; Earth Sciences ; Eddies ; Flow velocity ; Marine ; Mathematical models ; Meteorology ; Monsoons ; Ocean circulation ; Ocean currents ; Oceanography ; Sedimentation & deposition ; Temperature gradients ; Wind ; 东北季风 ; 中尺度 ; 冬季 ; 切变锋 ; 剪切带 ; 沉积作用 ; 沉积效应 ; 黄海暖流</subject><ispartof>Journal of Ocean University of China, 2016-02, Vol.15 (1), p.50-56</ispartof><rights>Science Press, Ocean University of China and Springer-Verlag Berlin Heidelberg 2016</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c412t-25b4211b1445cceefbcac14b9b15eae67f9a6c7dcdb7b6ccd83d7a3114b7fb4d3</citedby><cites>FETCH-LOGICAL-c412t-25b4211b1445cceefbcac14b9b15eae67f9a6c7dcdb7b6ccd83d7a3114b7fb4d3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/87473A/87473A.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11802-016-2668-7$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11802-016-2668-7$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids></links><search><creatorcontrib>Gao, Fei</creatorcontrib><creatorcontrib>Qiao, Lulu</creatorcontrib><creatorcontrib>Li, Guangxue</creatorcontrib><title>Winter Meso-Scale Shear Front in the Yellow Sea and Its Sedimentary Effects</title><title>Journal of Ocean University of China</title><addtitle>J. Ocean Univ. China</addtitle><addtitle>Journal of Ocean University of China</addtitle><description>In this paper, the authors explored the presence of shear fronts between the Yellow Sea Coastal Current （YSCC） and the monsoon-strengthened Yellow Sea Warm Current （YSWC） in winter and their sedimentary effects within the shear zone based on a fully validated numerical model. This work added the wind force to a tidal model during simulating the winter baroclinic circulation in the Yellow Sea. The results indicate that the YSWC is significantly strengthened by wind-driven compensation due to a northeast monsoon during winter time. When this warm current encounters the North Shandong-South Yellow Sea coastal current, there is a strong reverse shear action between the two current systems, forming a reverse-S-shaped shear front that begins near 34°N in the south and extends to approximately 38°N, with an overall length of over 600km. The main driving force for the formation of this shear front derives from the circulation system with the reverse flow. In the shear zone, temperature and salinity gradients increase, flow velocities are relatively small and the flow direction on one side of the shear zone is opposite to that on the other side. The ver- tical circulation structure is complicated, consisting of a series ofmeso- and small-scale anti-clockwise eddies. Particularly, this shear effect significantly hinders the horizontal exchange of coastal sediments carried by warm currents, resulting in fine sediments deposi- tion due to the weak hydrodynamic regime.</description><subject>Coastal currents</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Eddies</subject><subject>Flow velocity</subject><subject>Marine</subject><subject>Mathematical models</subject><subject>Meteorology</subject><subject>Monsoons</subject><subject>Ocean circulation</subject><subject>Ocean currents</subject><subject>Oceanography</subject><subject>Sedimentation & deposition</subject><subject>Temperature gradients</subject><subject>Wind</subject><subject>东北季风</subject><subject>中尺度</subject><subject>冬季</subject><subject>切变锋</subject><subject>剪切带</subject><subject>沉积作用</subject><subject>沉积效应</subject><subject>黄海暖流</subject><issn>1672-5182</issn><issn>1993-5021</issn><issn>1672-5174</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kUtPHDEQhEcoSDySH5CbBRekyInbz50jQpCgEHFYUJST5UfP7qBdD2vPCvj38WoQQjnk5D58VdWubprPwL4CY-ZbAZgxThloyrWeUbPXHELbCqoYhw911oZTBTN-0ByV8sCYEkqbw-bn7z6NmMkvLAOdB7dCMl-iy-QqD2kkfSLjEskfXK2GJzJHR1yK5HosdY79GtPo8gu57DoMY_nY7HduVfDT63vc3F9d3l38oDe3368vzm9okMBHypWXHMCDlCoExM4HF0D61oNCh9p0rdPBxBC98TqEOBPROAEVMZ2XURw3XybfJ5c6lxb2YdjmVBPtJi5f4vOzt8hrE2zXTKXPJvoxD5stltGu-xLqh1zCYVssGK1ao5QUFT39B31zBqM0E8pwWSmYqJCHUjJ29jH369qDBWZ3kXY6hq0r2N0x7G4JPmlKZdMC8zvn_4hOXoOWQ1psqu4tqQJMMhBK_AXEXJbY</recordid><startdate>20160201</startdate><enddate>20160201</enddate><creator>Gao, Fei</creator><creator>Qiao, Lulu</creator><creator>Li, Guangxue</creator><general>Science Press</general><general>Springer Nature B.V</general><general>Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology,Ministry of Land and Resources,Qingdao 266071,P.R.China%College of Marine Geosciences,Ocean University of China,Qingdao 266100,P.R.China</general><general>College of Marine Geosciences,Ocean University of China,Qingdao 266100,P.R.China</general><general>Qingdao Institute of Marine Geology,China Geological Survey,Qingdao 266071,P.R.China</general><general>Key Laboratory of Submarine Geoscience and Prospecti of Ministry of Education,Qingdao 266100,P.R.China</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7T7</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</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>FR3</scope><scope>GNUQQ</scope><scope>H95</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>P64</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>7TG</scope><scope>KL.</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20160201</creationdate><title>Winter Meso-Scale Shear Front in the Yellow Sea and Its Sedimentary Effects</title><author>Gao, Fei ; Qiao, Lulu ; Li, Guangxue</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c412t-25b4211b1445cceefbcac14b9b15eae67f9a6c7dcdb7b6ccd83d7a3114b7fb4d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Coastal currents</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Eddies</topic><topic>Flow velocity</topic><topic>Marine</topic><topic>Mathematical models</topic><topic>Meteorology</topic><topic>Monsoons</topic><topic>Ocean circulation</topic><topic>Ocean currents</topic><topic>Oceanography</topic><topic>Sedimentation & deposition</topic><topic>Temperature gradients</topic><topic>Wind</topic><topic>东北季风</topic><topic>中尺度</topic><topic>冬季</topic><topic>切变锋</topic><topic>剪切带</topic><topic>沉积作用</topic><topic>沉积效应</topic><topic>黄海暖流</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Gao, Fei</creatorcontrib><creatorcontrib>Qiao, Lulu</creatorcontrib><creatorcontrib>Li, Guangxue</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</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>Engineering Research Database</collection><collection>ProQuest Central Student</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>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Biotechnology and BioEngineering Abstracts</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>Meteorological & Geoastrophysical Abstracts - Academic</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>Gao, Fei</au><au>Qiao, Lulu</au><au>Li, Guangxue</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Winter Meso-Scale Shear Front in the Yellow Sea and Its Sedimentary Effects</atitle><jtitle>Journal of Ocean University of China</jtitle><stitle>J. Ocean Univ. China</stitle><addtitle>Journal of Ocean University of China</addtitle><date>2016-02-01</date><risdate>2016</risdate><volume>15</volume><issue>1</issue><spage>50</spage><epage>56</epage><pages>50-56</pages><issn>1672-5182</issn><eissn>1993-5021</eissn><eissn>1672-5174</eissn><abstract>In this paper, the authors explored the presence of shear fronts between the Yellow Sea Coastal Current （YSCC） and the monsoon-strengthened Yellow Sea Warm Current （YSWC） in winter and their sedimentary effects within the shear zone based on a fully validated numerical model. This work added the wind force to a tidal model during simulating the winter baroclinic circulation in the Yellow Sea. The results indicate that the YSWC is significantly strengthened by wind-driven compensation due to a northeast monsoon during winter time. When this warm current encounters the North Shandong-South Yellow Sea coastal current, there is a strong reverse shear action between the two current systems, forming a reverse-S-shaped shear front that begins near 34°N in the south and extends to approximately 38°N, with an overall length of over 600km. The main driving force for the formation of this shear front derives from the circulation system with the reverse flow. In the shear zone, temperature and salinity gradients increase, flow velocities are relatively small and the flow direction on one side of the shear zone is opposite to that on the other side. The ver- tical circulation structure is complicated, consisting of a series ofmeso- and small-scale anti-clockwise eddies. Particularly, this shear effect significantly hinders the horizontal exchange of coastal sediments carried by warm currents, resulting in fine sediments deposi- tion due to the weak hydrodynamic regime.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s11802-016-2668-7</doi><tpages>7</tpages></addata></record> |
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| source | Springer Nature - Complete Springer Journals; Alma/SFX Local Collection |
| subjects | Coastal currents Earth and Environmental Science Earth Sciences Eddies Flow velocity Marine Mathematical models Meteorology Monsoons Ocean circulation Ocean currents Oceanography Sedimentation & deposition Temperature gradients Wind 东北季风 中尺度 冬季 切变锋 剪切带 沉积作用 沉积效应 黄海暖流 |
| title | Winter Meso-Scale Shear Front in the Yellow Sea and Its Sedimentary Effects |
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