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        <identifier>oai:ir.kagoshima-u.ac.jp:00000764</identifier>
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          <dc:title xml:lang="en">Oceanic Conditions in the Western Tropical Pacific in the Summer of 1988</dc:title>
          <dc:title xml:lang="ja">1988年夏期 西部熱帯太平洋に於ける海況</dc:title>
          <jpcoar:creator>
            <jpcoar:creatorName xml:lang="en">YUWAKI, Yasutaka</jpcoar:creatorName>
            <jpcoar:creatorName xml:lang="ja">湯脇, 泰隆</jpcoar:creatorName>
          </jpcoar:creator>
          <jpcoar:creator>
            <jpcoar:creatorName xml:lang="en">NISHI, Toru</jpcoar:creatorName>
            <jpcoar:creatorName xml:lang="ja">西, 徹</jpcoar:creatorName>
          </jpcoar:creator>
          <jpcoar:creator>
            <jpcoar:creatorName xml:lang="en">MASUMITSU, Sunao</jpcoar:creatorName>
            <jpcoar:creatorName xml:lang="ja">益滿, 侃</jpcoar:creatorName>
          </jpcoar:creator>
          <jpcoar:creator>
            <jpcoar:creatorName xml:lang="en">HIGASHI, Masataka</jpcoar:creatorName>
            <jpcoar:creatorName xml:lang="ja">東, 政能</jpcoar:creatorName>
          </jpcoar:creator>
          <dcterms:accessRights rdf:resource="http://purl.org/coar/access_right/c_abf2">open access</dcterms:accessRights>
          <jpcoar:subject xml:lang="en" subjectScheme="Other">Oceanic condition</jpcoar:subject>
          <jpcoar:subject xml:lang="en" subjectScheme="Other">Western Tropical Pacific</jpcoar:subject>
          <jpcoar:subject xml:lang="en" subjectScheme="Other">Equatorial Current</jpcoar:subject>
          <datacite:description xml:lang="en" descriptionType="Other">Oceanographic observations using a CTD system were made in the Western Tropical Pacific
in the summer of 1988.
The first oceanographic section was made along 133°E from 20°N to 10°N from June 13-18th,
and the second one from 09°N, 138°E to 00°, 149°E from June 25-28th. The warm surface water
having a value of above 29°C was presented over the whole sea surface. The thermocline with
the maximum vertical gradient having a value of 0.17°C/m was the shallowest near 09°N. The
low salinity lower than 34.50% was presented in the surface mixed layer between 16°N and
02°N.
The conspicuous transitions were formed on each side of the north and south of the low salinity
water.
The North Equatorial Current was recognized on the north side of 08°N ; the South Equatorial
Current near the Equator ; and the North Equatorial Countercurrent in the region between 08°N
and 01°N. Several step-like features and inversion layers were presented in the thermocline at
the Equator. The lateral advection of water masses in the surface layer was well developed near
the Equator.</datacite:description>
          <dc:publisher xml:lang="ja">鹿児島大学</dc:publisher>
          <dc:publisher xml:lang="en">Kagoshima University</dc:publisher>
          <datacite:date dateType="Issued">1988-12-25</datacite:date>
          <dc:language>eng</dc:language>
          <dc:type rdf:resource="http://purl.org/coar/resource_type/c_6501">departmental bulletin paper</dc:type>
          <oaire:version rdf:resource="http://purl.org/coar/version/c_970fb48d4fbd8a85">VoR</oaire:version>
          <jpcoar:identifier identifierType="HDL">http://hdl.handle.net/10232/13373</jpcoar:identifier>
          <jpcoar:identifier identifierType="URI">https://ir.kagoshima-u.ac.jp/records/764</jpcoar:identifier>
          <jpcoar:sourceIdentifier identifierType="PISSN">0453087X</jpcoar:sourceIdentifier>
          <jpcoar:sourceIdentifier identifierType="NCID">AN00040498</jpcoar:sourceIdentifier>
          <jpcoar:sourceTitle xml:lang="ja">鹿児島大学水産学部紀要</jpcoar:sourceTitle>
          <jpcoar:sourceTitle xml:lang="en">Memoirs of Faculty of Fisheries Kagoshima University</jpcoar:sourceTitle>
          <jpcoar:volume>37</jpcoar:volume>
          <jpcoar:pageStart>97</jpcoar:pageStart>
          <jpcoar:pageEnd>109</jpcoar:pageEnd>
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            <datacite:date dateType="Available">2016-10-27</datacite:date>
            <datacite:date dateType="Issued">1988-12-25</datacite:date>
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