Seasonal Variations and Long-term Trends of the Coastal Upwelling along the Southwestern Coast of the East Sea/Japan Sea
Shin, C.-W.; Kim, D.G., and Jang, C.J., 2018. Seasonal variations and long-term trends of the coastal upwelling along the southwestern coast of the East Sea/Japan Sea. In: Shim, J.-S.; Chun, I., and Lim, H.S. (eds.), Proceedings from the International Coastal Symposium (ICS) 2018 (Busan, Republic of...
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description | Shin, C.-W.; Kim, D.G., and Jang, C.J., 2018. Seasonal variations and long-term trends of the coastal upwelling along the southwestern coast of the East Sea/Japan Sea. In: Shim, J.-S.; Chun, I., and Lim, H.S. (eds.), Proceedings from the International Coastal Symposium (ICS) 2018 (Busan, Republic of Korea). Journal of Coastal Research, Special Issue No. 85, pp. 471–475. Coconut Creek (Florida), ISSN 0749-0208. Southwesterly winds cause coastal upwelling along the southwestern coast of the East Sea/Japan Sea (EJS) in summer. To investigate the seasonal variations and long-term trends in the coastal upwelling, the observations of the Sea Surface Temperature (SST) at Gampo and the wind at Busan from 1968 to 2012 were analyzed. Upwelling signals estimated by temperature anomalies were negatively correlated (r ≈ −0.6) with southwesterly winds in summer. In addition, the signals were closely related to the Net Primary Production (NPP) near the upwelling region in late spring to early summer, which was the reason for the summer NPP peak in this area. The upwelling index driven by the wind shows that the upwelling would occur from April to August with a maximum strength in July. The long-term upwelling trends differed considerably according to the season: they increased in spring and decreased in summer, but the interannual variability in summer reduced the statistical confidence of the trends. |
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Seasonal variations and long-term trends of the coastal upwelling along the southwestern coast of the East Sea/Japan Sea. In: Shim, J.-S.; Chun, I., and Lim, H.S. (eds.), Proceedings from the International Coastal Symposium (ICS) 2018 (Busan, Republic of Korea). Journal of Coastal Research, Special Issue No. 85, pp. 471–475. Coconut Creek (Florida), ISSN 0749-0208. Southwesterly winds cause coastal upwelling along the southwestern coast of the East Sea/Japan Sea (EJS) in summer. To investigate the seasonal variations and long-term trends in the coastal upwelling, the observations of the Sea Surface Temperature (SST) at Gampo and the wind at Busan from 1968 to 2012 were analyzed. Upwelling signals estimated by temperature anomalies were negatively correlated (r ≈ −0.6) with southwesterly winds in summer. In addition, the signals were closely related to the Net Primary Production (NPP) near the upwelling region in late spring to early summer, which was the reason for the summer NPP peak in this area. The upwelling index driven by the wind shows that the upwelling would occur from April to August with a maximum strength in July. The long-term upwelling trends differed considerably according to the season: they increased in spring and decreased in summer, but the interannual variability in summer reduced the statistical confidence of the trends.</description><identifier>ISSN: 0749-0208</identifier><identifier>EISSN: 1551-5036</identifier><identifier>DOI: 10.2112/SI85-095.1</identifier><language>eng</language><publisher>Fort Lauderdale: Coastal Education and Research Foundation</publisher><subject>Anomalies ; blooming ; Chlorophyll ; Climate change ; Coastal upwelling ; Coasts ; Cold ; Confidence intervals ; CONTINENTAL SHELVES AND SLOPES ; Ecosystems ; Global warming ; High temperature ; monsoon ; net primary production ; Ocean circulation ; Oceanography ; Primary production ; Sea surface ; Sea surface temperature ; Seasonal variation ; Seasonal variations ; Seasons ; Spring ; Summer ; Temperature anomalies ; Trends ; Upwelling ; Upwelling index ; Wind ; Winds</subject><ispartof>Journal of coastal research, 2018-05, Vol.85 (sp1), p.471-475</ispartof><rights>Coastal Education and Research Foundation, Inc. 2018</rights><rights>Copyright Allen Press Publishing Services 2018</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-b314t-1be356be5c68ae4bb9f735152d15fb16535f21550df052344868db5057e45bb63</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/26488262$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/26488262$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,27901,27902,57992,58225</link.rule.ids></links><search><creatorcontrib>Shin, Chang-Woong</creatorcontrib><creatorcontrib>Kim, Dong Guk</creatorcontrib><creatorcontrib>Jang, Chan Joo</creatorcontrib><title>Seasonal Variations and Long-term Trends of the Coastal Upwelling along the Southwestern Coast of the East Sea/Japan Sea</title><title>Journal of coastal research</title><description>Shin, C.-W.; Kim, D.G., and Jang, C.J., 2018. Seasonal variations and long-term trends of the coastal upwelling along the southwestern coast of the East Sea/Japan Sea. In: Shim, J.-S.; Chun, I., and Lim, H.S. (eds.), Proceedings from the International Coastal Symposium (ICS) 2018 (Busan, Republic of Korea). Journal of Coastal Research, Special Issue No. 85, pp. 471–475. Coconut Creek (Florida), ISSN 0749-0208. Southwesterly winds cause coastal upwelling along the southwestern coast of the East Sea/Japan Sea (EJS) in summer. To investigate the seasonal variations and long-term trends in the coastal upwelling, the observations of the Sea Surface Temperature (SST) at Gampo and the wind at Busan from 1968 to 2012 were analyzed. Upwelling signals estimated by temperature anomalies were negatively correlated (r ≈ −0.6) with southwesterly winds in summer. In addition, the signals were closely related to the Net Primary Production (NPP) near the upwelling region in late spring to early summer, which was the reason for the summer NPP peak in this area. The upwelling index driven by the wind shows that the upwelling would occur from April to August with a maximum strength in July. The long-term upwelling trends differed considerably according to the season: they increased in spring and decreased in summer, but the interannual variability in summer reduced the statistical confidence of the trends.</description><subject>Anomalies</subject><subject>blooming</subject><subject>Chlorophyll</subject><subject>Climate change</subject><subject>Coastal upwelling</subject><subject>Coasts</subject><subject>Cold</subject><subject>Confidence intervals</subject><subject>CONTINENTAL SHELVES AND SLOPES</subject><subject>Ecosystems</subject><subject>Global warming</subject><subject>High temperature</subject><subject>monsoon</subject><subject>net primary production</subject><subject>Ocean circulation</subject><subject>Oceanography</subject><subject>Primary production</subject><subject>Sea surface</subject><subject>Sea surface temperature</subject><subject>Seasonal variation</subject><subject>Seasonal variations</subject><subject>Seasons</subject><subject>Spring</subject><subject>Summer</subject><subject>Temperature anomalies</subject><subject>Trends</subject><subject>Upwelling</subject><subject>Upwelling index</subject><subject>Wind</subject><subject>Winds</subject><issn>0749-0208</issn><issn>1551-5036</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kM1LwzAYxoMoOKcX70LAiwjdkjRv2h5lTJ0MPGzzWpI13Tq6pCYd0__e1KpHT-8Dz-_9ehC6pmTEKGXjxSyFiGQwoidoQAFoBCQWp2hAEp5FhJH0HF14vyOEipQnA_Sx0NJbI2v8Jl0l28oaj6Up8NyaTdRqt8dLp03hsS1xu9V4YqVvA75qjrquK7PBsg7ot7ewh3Z71D60mR787Zp2Oqwav8hGmk5dorNS1l5f_dQhWj1Ol5PnaP76NJs8zCMVU95GVOkYhNKwFqnUXKmsTGKgwAoKpaICYihZeJQUJQEWc56KtFBAINEclBLxEN32cxtn3w_htnxnDy487HNGMsazOKEQqPueWjvrvdNl3rhqL91nTkneJZt3yeYh2ZwG-KaHd7617o9kgqcpEyz4d72vKmuN_m_UF2fAgOU</recordid><startdate>20180501</startdate><enddate>20180501</enddate><creator>Shin, Chang-Woong</creator><creator>Kim, Dong Guk</creator><creator>Jang, Chan Joo</creator><general>Coastal Education and Research Foundation</general><general>COASTAL EDUCATION & RESEARCH FOUNDATION, INC. 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Variations and Long-term Trends of the Coastal Upwelling along the Southwestern Coast of the East Sea/Japan Sea</title><author>Shin, Chang-Woong ; Kim, Dong Guk ; Jang, Chan Joo</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-b314t-1be356be5c68ae4bb9f735152d15fb16535f21550df052344868db5057e45bb63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Anomalies</topic><topic>blooming</topic><topic>Chlorophyll</topic><topic>Climate change</topic><topic>Coastal upwelling</topic><topic>Coasts</topic><topic>Cold</topic><topic>Confidence intervals</topic><topic>CONTINENTAL SHELVES AND SLOPES</topic><topic>Ecosystems</topic><topic>Global warming</topic><topic>High temperature</topic><topic>monsoon</topic><topic>net primary production</topic><topic>Ocean circulation</topic><topic>Oceanography</topic><topic>Primary production</topic><topic>Sea surface</topic><topic>Sea surface 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research</jtitle><date>2018-05-01</date><risdate>2018</risdate><volume>85</volume><issue>sp1</issue><spage>471</spage><epage>475</epage><pages>471-475</pages><issn>0749-0208</issn><eissn>1551-5036</eissn><abstract>Shin, C.-W.; Kim, D.G., and Jang, C.J., 2018. Seasonal variations and long-term trends of the coastal upwelling along the southwestern coast of the East Sea/Japan Sea. In: Shim, J.-S.; Chun, I., and Lim, H.S. (eds.), Proceedings from the International Coastal Symposium (ICS) 2018 (Busan, Republic of Korea). Journal of Coastal Research, Special Issue No. 85, pp. 471–475. Coconut Creek (Florida), ISSN 0749-0208. Southwesterly winds cause coastal upwelling along the southwestern coast of the East Sea/Japan Sea (EJS) in summer. To investigate the seasonal variations and long-term trends in the coastal upwelling, the observations of the Sea Surface Temperature (SST) at Gampo and the wind at Busan from 1968 to 2012 were analyzed. Upwelling signals estimated by temperature anomalies were negatively correlated (r ≈ −0.6) with southwesterly winds in summer. In addition, the signals were closely related to the Net Primary Production (NPP) near the upwelling region in late spring to early summer, which was the reason for the summer NPP peak in this area. The upwelling index driven by the wind shows that the upwelling would occur from April to August with a maximum strength in July. The long-term upwelling trends differed considerably according to the season: they increased in spring and decreased in summer, but the interannual variability in summer reduced the statistical confidence of the trends.</abstract><cop>Fort Lauderdale</cop><pub>Coastal Education and Research Foundation</pub><doi>10.2112/SI85-095.1</doi><tpages>5</tpages></addata></record> |
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subjects | Anomalies blooming Chlorophyll Climate change Coastal upwelling Coasts Cold Confidence intervals CONTINENTAL SHELVES AND SLOPES Ecosystems Global warming High temperature monsoon net primary production Ocean circulation Oceanography Primary production Sea surface Sea surface temperature Seasonal variation Seasonal variations Seasons Spring Summer Temperature anomalies Trends Upwelling Upwelling index Wind Winds |
title | Seasonal Variations and Long-term Trends of the Coastal Upwelling along the Southwestern Coast of the East Sea/Japan Sea |
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