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Study on the Behavior of the Water Temperature Inversion Layer in the Northern East China Sea
To investigate the behavioral characteristics of the water temperature inversion layer (TIL), we used data (KODC) from areas in the Northern East China Sea from 1995 to 2016. Water temperature and salinity surveys were conducted 8820 casts over 22 years. Of these, 1589 water temperature inversion la...
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Published in: | Journal of marine science and engineering 2020-03, Vol.8 (3), p.157 |
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description | To investigate the behavioral characteristics of the water temperature inversion layer (TIL), we used data (KODC) from areas in the Northern East China Sea from 1995 to 2016. Water temperature and salinity surveys were conducted 8820 casts over 22 years. Of these, 1589 water temperature inversion layers were found, and the probability of occurrence was 18.0%. In the Gageo island, probability of TIL occurrence in winter was 25 times higher than in summer. On the other hand, in the south of Jeju Island, summer values were 3.7 times higher than winter values. A T–S diagram analysis shows the components of the water temperature inversion layers. Yellow Sea Cold Water was mainly found in the winter, while Jeju Warm Currents and Tsushima Warm Currents were found in summer. The correlation between the probability of the occurrence of a monthly water temperature inversion layer and the amount of seawater volume transported into the study area was analyzed. The correlation coefficient was higher than r = 0.8 in parts of southern Jeju Island. On the other hand, the correlation coefficient was r = −0.6 in the Gageo Island. The spatial correlation index for the seawater volume transport and the water temperature inversion layer is presented. |
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Water temperature and salinity surveys were conducted 8820 casts over 22 years. Of these, 1589 water temperature inversion layers were found, and the probability of occurrence was 18.0%. In the Gageo island, probability of TIL occurrence in winter was 25 times higher than in summer. On the other hand, in the south of Jeju Island, summer values were 3.7 times higher than winter values. A T–S diagram analysis shows the components of the water temperature inversion layers. Yellow Sea Cold Water was mainly found in the winter, while Jeju Warm Currents and Tsushima Warm Currents were found in summer. The correlation between the probability of the occurrence of a monthly water temperature inversion layer and the amount of seawater volume transported into the study area was analyzed. The correlation coefficient was higher than r = 0.8 in parts of southern Jeju Island. On the other hand, the correlation coefficient was r = −0.6 in the Gageo Island. The spatial correlation index for the seawater volume transport and the water temperature inversion layer is presented.</description><identifier>ISSN: 2077-1312</identifier><identifier>EISSN: 2077-1312</identifier><identifier>DOI: 10.3390/jmse8030157</identifier><language>eng</language><publisher>MDPI AG</publisher><subject>jeju island ; jeju warm current ; northern east china sea ; tsushima warm current ; volume transport ; water temperature inversion layer ; yellow sea cold water</subject><ispartof>Journal of marine science and engineering, 2020-03, Vol.8 (3), p.157</ispartof><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c266t-ca3f35677cbdec556a851b982c1ba80df9e5336ccef406f6b73560c51f9c5153</citedby><cites>FETCH-LOGICAL-c266t-ca3f35677cbdec556a851b982c1ba80df9e5336ccef406f6b73560c51f9c5153</cites><orcidid>0000-0002-8665-3146 ; 0000-0003-2438-7572</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Kim, Seong Hyeon</creatorcontrib><creatorcontrib>Choi, Bok Kyoung</creatorcontrib><creatorcontrib>Kim, Eung</creatorcontrib><title>Study on the Behavior of the Water Temperature Inversion Layer in the Northern East China Sea</title><title>Journal of marine science and engineering</title><description>To investigate the behavioral characteristics of the water temperature inversion layer (TIL), we used data (KODC) from areas in the Northern East China Sea from 1995 to 2016. Water temperature and salinity surveys were conducted 8820 casts over 22 years. Of these, 1589 water temperature inversion layers were found, and the probability of occurrence was 18.0%. In the Gageo island, probability of TIL occurrence in winter was 25 times higher than in summer. On the other hand, in the south of Jeju Island, summer values were 3.7 times higher than winter values. A T–S diagram analysis shows the components of the water temperature inversion layers. Yellow Sea Cold Water was mainly found in the winter, while Jeju Warm Currents and Tsushima Warm Currents were found in summer. The correlation between the probability of the occurrence of a monthly water temperature inversion layer and the amount of seawater volume transported into the study area was analyzed. The correlation coefficient was higher than r = 0.8 in parts of southern Jeju Island. On the other hand, the correlation coefficient was r = −0.6 in the Gageo Island. The spatial correlation index for the seawater volume transport and the water temperature inversion layer is presented.</description><subject>jeju island</subject><subject>jeju warm current</subject><subject>northern east china sea</subject><subject>tsushima warm current</subject><subject>volume transport</subject><subject>water temperature inversion layer</subject><subject>yellow sea cold water</subject><issn>2077-1312</issn><issn>2077-1312</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>DOA</sourceid><recordid>eNpNkE1PAjEQhhujiQQ5-Qd6N6vtdvuxRyWoJEQPkHgym9nuVEpgS9qFhH_vAsYwh_l85zm8hNxz9ihEyZ5Wm4SGCcalviKDnGmdccHz64v-loxSWrE-TK44UwPyPe92zYGGlnZLpC-4hL0PkQZ3mr-gw0gXuNlihG4XkU7bPcbke_0MDv3Nnx8_QuxLbOkEUkfHS98CnSPckRsH64Sjvzoki9fJYvyezT7fpuPnWWZzpbrMgnBCKq1t3aCVUoGRvC5NbnkNhjWuRCmEshZdwZRTte7VzEruyj5JMSTTM7YJsKq20W8gHqoAvjotQvypIHberrGqjdbKmbopUBWssLVFa6UpeN5goTnrWQ9nlo0hpYjun8dZdfS5uvBZ_ALP2XCJ</recordid><startdate>20200301</startdate><enddate>20200301</enddate><creator>Kim, Seong Hyeon</creator><creator>Choi, Bok Kyoung</creator><creator>Kim, Eung</creator><general>MDPI AG</general><scope>AAYXX</scope><scope>CITATION</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0002-8665-3146</orcidid><orcidid>https://orcid.org/0000-0003-2438-7572</orcidid></search><sort><creationdate>20200301</creationdate><title>Study on the Behavior of the Water Temperature Inversion Layer in the Northern East China Sea</title><author>Kim, Seong Hyeon ; Choi, Bok Kyoung ; Kim, Eung</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c266t-ca3f35677cbdec556a851b982c1ba80df9e5336ccef406f6b73560c51f9c5153</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>jeju island</topic><topic>jeju warm current</topic><topic>northern east china sea</topic><topic>tsushima warm current</topic><topic>volume transport</topic><topic>water temperature inversion layer</topic><topic>yellow sea cold water</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kim, Seong Hyeon</creatorcontrib><creatorcontrib>Choi, Bok Kyoung</creatorcontrib><creatorcontrib>Kim, Eung</creatorcontrib><collection>CrossRef</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>Journal of marine science and engineering</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kim, Seong Hyeon</au><au>Choi, Bok Kyoung</au><au>Kim, Eung</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Study on the Behavior of the Water Temperature Inversion Layer in the Northern East China Sea</atitle><jtitle>Journal of marine science and engineering</jtitle><date>2020-03-01</date><risdate>2020</risdate><volume>8</volume><issue>3</issue><spage>157</spage><pages>157-</pages><issn>2077-1312</issn><eissn>2077-1312</eissn><abstract>To investigate the behavioral characteristics of the water temperature inversion layer (TIL), we used data (KODC) from areas in the Northern East China Sea from 1995 to 2016. Water temperature and salinity surveys were conducted 8820 casts over 22 years. Of these, 1589 water temperature inversion layers were found, and the probability of occurrence was 18.0%. In the Gageo island, probability of TIL occurrence in winter was 25 times higher than in summer. On the other hand, in the south of Jeju Island, summer values were 3.7 times higher than winter values. A T–S diagram analysis shows the components of the water temperature inversion layers. Yellow Sea Cold Water was mainly found in the winter, while Jeju Warm Currents and Tsushima Warm Currents were found in summer. The correlation between the probability of the occurrence of a monthly water temperature inversion layer and the amount of seawater volume transported into the study area was analyzed. The correlation coefficient was higher than r = 0.8 in parts of southern Jeju Island. On the other hand, the correlation coefficient was r = −0.6 in the Gageo Island. 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subjects | jeju island jeju warm current northern east china sea tsushima warm current volume transport water temperature inversion layer yellow sea cold water |
title | Study on the Behavior of the Water Temperature Inversion Layer in the Northern East China Sea |
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