Current structure and volume transport of the Soya Warm Current in summer
ADCP, CTD and XBT observations were conducted to investigate the current structure and temperature, salinity and density distributions in the Soya Warm Current (SWC) in August, 1998 and July, 2000. The ADCP observations clearly revealed the SWC along the Hokkaido coast, with a width of 30-35 km and...
Gespeichert in:
| Veröffentlicht in: | Journal of oceanography 2006-04, Vol.62 (2), p.197-205 |
|---|---|
| Hauptverfasser: | , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 205 |
|---|---|
| container_issue | 2 |
| container_start_page | 197 |
| container_title | Journal of oceanography |
| container_volume | 62 |
| creator | Matsuyama, Masaji Wadaka, Makiko Abe, Taizo Aota, Masaaki Koike, Yoshio |
| description | ADCP, CTD and XBT observations were conducted to investigate the current structure and temperature, salinity and density distributions in the Soya Warm Current (SWC) in August, 1998 and July, 2000. The ADCP observations clearly revealed the SWC along the Hokkaido coast, with a width of 30-35 km and an axis of maximum speed of 1.0 to 1.3 ms^sup -1^, located at 20-25 km from the coast. The current speed gradually increased from the coast to a maximum and steeply decreased in the offshore direction. The SWC consisted of both barotropic and baroclinic components, and the existence of the baroclinic component was confirmed by both the density front near the current axis and vertical shear of the alongshore current. The baroclinic component strengthened the barotropic component in the upper layer near the axis of the SWC. The volume transport of the SWC was 1.2-1.3 SV in August, 1998 and about 1.5 SV and July, 2000, respectively. Of the total transport, 13 to 15% was taken up by the baroclinic component. A weak southeastward current was found off the SWC. It had barotropic characteristics, and is surmised to be a part of the East Sakhalin Current.[PUBLICATION ABSTRACT] |
| doi_str_mv | 10.1007/s10872-006-0044-8 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest</sourceid><recordid>TN_cdi_proquest_miscellaneous_20987525</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>20987525</sourcerecordid><originalsourceid>FETCH-LOGICAL-p143t-c57b773d13987eb2cce65d30e78eed38409c7e575932ddcb512d024be6b20f03</originalsourceid><addsrcrecordid>eNpdj01LAzEYhIMoWKs_wFvw4C36Jtl87FGK1kLBgwW9LbvJW2zZ3dR8CP57V9SLh2EuM8MzhFxyuOEA5jZxsEYwAD2pqpg9IjOujGRW29djMoOaa2algVNyltIeAGpr5IysFiVGHDNNORaXS0Tajp5-hL4MSHNsx3QIMdOwpfkN6XP4bOlLGwf619uNNJVhwHhOTrZtn_Di1-dk83C_WTyy9dNytbhbswOvZGZOmc4Y6bmcALATzqFWXgIai-ilraB2BpVRtRTeu05x4UFUHepOwBbknFz_zB5ieC-YcjPsksO-b0cMJTXi-5gSagpe_QvuQ4njhNYYxSttuNLyC_bIXBo</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>751467156</pqid></control><display><type>article</type><title>Current structure and volume transport of the Soya Warm Current in summer</title><source>Springer Online Journals Complete</source><source>Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals</source><source>Alma/SFX Local Collection</source><creator>Matsuyama, Masaji ; Wadaka, Makiko ; Abe, Taizo ; Aota, Masaaki ; Koike, Yoshio</creator><creatorcontrib>Matsuyama, Masaji ; Wadaka, Makiko ; Abe, Taizo ; Aota, Masaaki ; Koike, Yoshio</creatorcontrib><description>ADCP, CTD and XBT observations were conducted to investigate the current structure and temperature, salinity and density distributions in the Soya Warm Current (SWC) in August, 1998 and July, 2000. The ADCP observations clearly revealed the SWC along the Hokkaido coast, with a width of 30-35 km and an axis of maximum speed of 1.0 to 1.3 ms^sup -1^, located at 20-25 km from the coast. The current speed gradually increased from the coast to a maximum and steeply decreased in the offshore direction. The SWC consisted of both barotropic and baroclinic components, and the existence of the baroclinic component was confirmed by both the density front near the current axis and vertical shear of the alongshore current. The baroclinic component strengthened the barotropic component in the upper layer near the axis of the SWC. The volume transport of the SWC was 1.2-1.3 SV in August, 1998 and about 1.5 SV and July, 2000, respectively. Of the total transport, 13 to 15% was taken up by the baroclinic component. A weak southeastward current was found off the SWC. It had barotropic characteristics, and is surmised to be a part of the East Sakhalin Current.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 0916-8370</identifier><identifier>EISSN: 1573-868X</identifier><identifier>DOI: 10.1007/s10872-006-0044-8</identifier><language>eng</language><publisher>Tokyo: Springer Nature B.V</publisher><subject>Marine ; Ocean circulation ; Ocean currents ; Oceanography</subject><ispartof>Journal of oceanography, 2006-04, Vol.62 (2), p.197-205</ispartof><rights>The Oceanographic Society of Japan/TERRAPUB/Springer 2006</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,781,785,27929,27930</link.rule.ids></links><search><creatorcontrib>Matsuyama, Masaji</creatorcontrib><creatorcontrib>Wadaka, Makiko</creatorcontrib><creatorcontrib>Abe, Taizo</creatorcontrib><creatorcontrib>Aota, Masaaki</creatorcontrib><creatorcontrib>Koike, Yoshio</creatorcontrib><title>Current structure and volume transport of the Soya Warm Current in summer</title><title>Journal of oceanography</title><description>ADCP, CTD and XBT observations were conducted to investigate the current structure and temperature, salinity and density distributions in the Soya Warm Current (SWC) in August, 1998 and July, 2000. The ADCP observations clearly revealed the SWC along the Hokkaido coast, with a width of 30-35 km and an axis of maximum speed of 1.0 to 1.3 ms^sup -1^, located at 20-25 km from the coast. The current speed gradually increased from the coast to a maximum and steeply decreased in the offshore direction. The SWC consisted of both barotropic and baroclinic components, and the existence of the baroclinic component was confirmed by both the density front near the current axis and vertical shear of the alongshore current. The baroclinic component strengthened the barotropic component in the upper layer near the axis of the SWC. The volume transport of the SWC was 1.2-1.3 SV in August, 1998 and about 1.5 SV and July, 2000, respectively. Of the total transport, 13 to 15% was taken up by the baroclinic component. A weak southeastward current was found off the SWC. It had barotropic characteristics, and is surmised to be a part of the East Sakhalin Current.[PUBLICATION ABSTRACT]</description><subject>Marine</subject><subject>Ocean circulation</subject><subject>Ocean currents</subject><subject>Oceanography</subject><issn>0916-8370</issn><issn>1573-868X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</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>eNpdj01LAzEYhIMoWKs_wFvw4C36Jtl87FGK1kLBgwW9LbvJW2zZ3dR8CP57V9SLh2EuM8MzhFxyuOEA5jZxsEYwAD2pqpg9IjOujGRW29djMoOaa2algVNyltIeAGpr5IysFiVGHDNNORaXS0Tajp5-hL4MSHNsx3QIMdOwpfkN6XP4bOlLGwf619uNNJVhwHhOTrZtn_Di1-dk83C_WTyy9dNytbhbswOvZGZOmc4Y6bmcALATzqFWXgIai-ilraB2BpVRtRTeu05x4UFUHepOwBbknFz_zB5ieC-YcjPsksO-b0cMJTXi-5gSagpe_QvuQ4njhNYYxSttuNLyC_bIXBo</recordid><startdate>20060401</startdate><enddate>20060401</enddate><creator>Matsuyama, Masaji</creator><creator>Wadaka, Makiko</creator><creator>Abe, Taizo</creator><creator>Aota, Masaaki</creator><creator>Koike, Yoshio</creator><general>Springer Nature B.V</general><scope>3V.</scope><scope>7ST</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</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>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><scope>7TG</scope><scope>KL.</scope></search><sort><creationdate>20060401</creationdate><title>Current structure and volume transport of the Soya Warm Current in summer</title><author>Matsuyama, Masaji ; Wadaka, Makiko ; Abe, Taizo ; Aota, Masaaki ; Koike, Yoshio</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p143t-c57b773d13987eb2cce65d30e78eed38409c7e575932ddcb512d024be6b20f03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Marine</topic><topic>Ocean circulation</topic><topic>Ocean currents</topic><topic>Oceanography</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Matsuyama, Masaji</creatorcontrib><creatorcontrib>Wadaka, Makiko</creatorcontrib><creatorcontrib>Abe, Taizo</creatorcontrib><creatorcontrib>Aota, Masaaki</creatorcontrib><creatorcontrib>Koike, Yoshio</creatorcontrib><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Oceanic 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 Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</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>Environmental Science Database</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>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><jtitle>Journal of oceanography</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Matsuyama, Masaji</au><au>Wadaka, Makiko</au><au>Abe, Taizo</au><au>Aota, Masaaki</au><au>Koike, Yoshio</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Current structure and volume transport of the Soya Warm Current in summer</atitle><jtitle>Journal of oceanography</jtitle><date>2006-04-01</date><risdate>2006</risdate><volume>62</volume><issue>2</issue><spage>197</spage><epage>205</epage><pages>197-205</pages><issn>0916-8370</issn><eissn>1573-868X</eissn><abstract>ADCP, CTD and XBT observations were conducted to investigate the current structure and temperature, salinity and density distributions in the Soya Warm Current (SWC) in August, 1998 and July, 2000. The ADCP observations clearly revealed the SWC along the Hokkaido coast, with a width of 30-35 km and an axis of maximum speed of 1.0 to 1.3 ms^sup -1^, located at 20-25 km from the coast. The current speed gradually increased from the coast to a maximum and steeply decreased in the offshore direction. The SWC consisted of both barotropic and baroclinic components, and the existence of the baroclinic component was confirmed by both the density front near the current axis and vertical shear of the alongshore current. The baroclinic component strengthened the barotropic component in the upper layer near the axis of the SWC. The volume transport of the SWC was 1.2-1.3 SV in August, 1998 and about 1.5 SV and July, 2000, respectively. Of the total transport, 13 to 15% was taken up by the baroclinic component. A weak southeastward current was found off the SWC. It had barotropic characteristics, and is surmised to be a part of the East Sakhalin Current.[PUBLICATION ABSTRACT]</abstract><cop>Tokyo</cop><pub>Springer Nature B.V</pub><doi>10.1007/s10872-006-0044-8</doi><tpages>9</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0916-8370 |
| ispartof | Journal of oceanography, 2006-04, Vol.62 (2), p.197-205 |
| issn | 0916-8370 1573-868X |
| language | eng |
| recordid | cdi_proquest_miscellaneous_20987525 |
| source | Springer Online Journals Complete; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Alma/SFX Local Collection |
| subjects | Marine Ocean circulation Ocean currents Oceanography |
| title | Current structure and volume transport of the Soya Warm Current in summer |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-15T11%3A31%3A04IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Current%20structure%20and%20volume%20transport%20of%20the%20Soya%20Warm%20Current%20in%20summer&rft.jtitle=Journal%20of%20oceanography&rft.au=Matsuyama,%20Masaji&rft.date=2006-04-01&rft.volume=62&rft.issue=2&rft.spage=197&rft.epage=205&rft.pages=197-205&rft.issn=0916-8370&rft.eissn=1573-868X&rft_id=info:doi/10.1007/s10872-006-0044-8&rft_dat=%3Cproquest%3E20987525%3C/proquest%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=751467156&rft_id=info:pmid/&rfr_iscdi=true |