Physical oceanographic conditions around the S1 mooring site
We describe physical oceanographic conditions around the S1 biogeochemical mooring site (30°N, 145°E) between February 2010 and July 2013. At the S1 mooring site, there is a clear seasonal variability of the mixed layer depth, wind forcing as well as horizontal kinetic energy in a near-inertial band...
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Veröffentlicht in: | Journal of oceanography 2016-06, Vol.72 (3), p.453-464 |
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creator | Inoue, Ryuichiro Kouketsu, Shinya |
description | We describe physical oceanographic conditions around the S1 biogeochemical mooring site (30°N, 145°E) between February 2010 and July 2013. At the S1 mooring site, there is a clear seasonal variability of the mixed layer depth, wind forcing as well as horizontal kinetic energy in a near-inertial band. Interannual variability of the winter mixed layer was observed. The winter mixed layer depth was shallower in early 2010 and became deeper afterwards. Several mesoscale eddies and typhoons passed by the S1 mooring sites every year. Based on observed events, we suggest that those physical processes possibly affected biogeochemical properties around the S1 mooring site. |
doi_str_mv | 10.1007/s10872-015-0342-0 |
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Based on observed events, we suggest that those physical processes possibly affected biogeochemical properties around the S1 mooring site.</description><identifier>ISSN: 0916-8370</identifier><identifier>EISSN: 1573-868X</identifier><identifier>DOI: 10.1007/s10872-015-0342-0</identifier><language>eng</language><publisher>Tokyo: Springer Japan</publisher><subject>Biogeochemistry ; Earth and Environmental Science ; Earth Sciences ; Eddies ; Freshwater & Marine Ecology ; Kinetic energy ; Marine ; Oceanography ; Physical oceanography ; Seasonal variations ; Special Section: Original Article ; Typhoons ; Winter</subject><ispartof>Journal of oceanography, 2016-06, Vol.72 (3), p.453-464</ispartof><rights>The Oceanographic Society of Japan and Springer Japan 2015</rights><rights>The Oceanographic Society of Japan and Springer Japan 2016</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c442t-7ad14854b2496ba3be9c7b80fc1bd0238f18cf9111a8478c3d01f2cd5f9c1db03</citedby><cites>FETCH-LOGICAL-c442t-7ad14854b2496ba3be9c7b80fc1bd0238f18cf9111a8478c3d01f2cd5f9c1db03</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10872-015-0342-0$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10872-015-0342-0$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Inoue, Ryuichiro</creatorcontrib><creatorcontrib>Kouketsu, Shinya</creatorcontrib><title>Physical oceanographic conditions around the S1 mooring site</title><title>Journal of oceanography</title><addtitle>J Oceanogr</addtitle><description>We describe physical oceanographic conditions around the S1 biogeochemical mooring site (30°N, 145°E) between February 2010 and July 2013. At the S1 mooring site, there is a clear seasonal variability of the mixed layer depth, wind forcing as well as horizontal kinetic energy in a near-inertial band. Interannual variability of the winter mixed layer was observed. The winter mixed layer depth was shallower in early 2010 and became deeper afterwards. Several mesoscale eddies and typhoons passed by the S1 mooring sites every year. Based on observed events, we suggest that those physical processes possibly affected biogeochemical properties around the S1 mooring site.</description><subject>Biogeochemistry</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Eddies</subject><subject>Freshwater & Marine Ecology</subject><subject>Kinetic energy</subject><subject>Marine</subject><subject>Oceanography</subject><subject>Physical oceanography</subject><subject>Seasonal variations</subject><subject>Special Section: Original Article</subject><subject>Typhoons</subject><subject>Winter</subject><issn>0916-8370</issn><issn>1573-868X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kE1LxDAURYMoOI7-AHcFN26q7zVpk4IbEb9gQEEFdyFNk5kMnaYm7WL-vS11IYKr9xbnXi6HkHOEKwTg1xFB8CwFzFOgbHwOyAJzTlNRiM9DsoASi1RQDsfkJMYtAJSC0wW5ed3so9OqSbw2qvXroLqN04n2be1659uYqOCHtk76jUneMNl5H1y7TqLrzSk5sqqJ5uznLsnHw_373VO6enl8vrtdpZqxrE-5qpGJnFUZK4tK0cqUmlcCrMaqhowKi0LbEhGVYFxoWgPaTNe5LTXWFdAluZx7u-C_BhN7uXNRm6ZRrfFDlChAFExwTkf04g-69UNox3USeTnqoTljI4UzpYOPMRgru-B2Kuwlgpx8ytmnHANy8imnEdmcid0kwIRfzf-GvgGjs3cY</recordid><startdate>20160601</startdate><enddate>20160601</enddate><creator>Inoue, Ryuichiro</creator><creator>Kouketsu, Shinya</creator><general>Springer Japan</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</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>20160601</creationdate><title>Physical oceanographic conditions around the S1 mooring site</title><author>Inoue, Ryuichiro ; 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At the S1 mooring site, there is a clear seasonal variability of the mixed layer depth, wind forcing as well as horizontal kinetic energy in a near-inertial band. Interannual variability of the winter mixed layer was observed. The winter mixed layer depth was shallower in early 2010 and became deeper afterwards. Several mesoscale eddies and typhoons passed by the S1 mooring sites every year. Based on observed events, we suggest that those physical processes possibly affected biogeochemical properties around the S1 mooring site.</abstract><cop>Tokyo</cop><pub>Springer Japan</pub><doi>10.1007/s10872-015-0342-0</doi><tpages>12</tpages></addata></record> |
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source | Alma/SFX Local Collection; SpringerLink Journals - AutoHoldings |
subjects | Biogeochemistry Earth and Environmental Science Earth Sciences Eddies Freshwater & Marine Ecology Kinetic energy Marine Oceanography Physical oceanography Seasonal variations Special Section: Original Article Typhoons Winter |
title | Physical oceanographic conditions around the S1 mooring site |
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