East Asian monsoon to El Niño/Southern Oscillation: A shift in the winter climate of Ishigaki Island accompanying the 1988/1989 regime shift, based on instrumental and coral records
The relationship between the coral skeletal oxygen isotope ratio (δ18Ocoral) of a coral core (Porites sp.), which was collected from the inshore area of Ishigaki Island, Japan (24°N, 124°E) and represents 180 years of continuous growth, and sea surface temperature (SST) was examined for the last 30...
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description | The relationship between the coral skeletal oxygen isotope ratio (δ18Ocoral) of a coral core (Porites sp.), which was collected from the inshore area of Ishigaki Island, Japan (24°N, 124°E) and represents 180 years of continuous growth, and sea surface temperature (SST) was examined for the last 30 years. A significant linear correlation was found between winter δ18Ocoral and SST measured at Ishigaki Port (SSTI), which suggests that the winter data from this coral sample is a good proxy for reconstructing past climate change. Furthermore, the winter instrumental SSTI shifted from being related to the East Asian Winter Monsoon to being dependent on the El Niño/Southern Oscillation in response to the 1988/1989 climate regime shift. Since this shift is also captured by the winter δ18Ocoral values, this 180‐year coral core record may provide insight into past climate regime shifts that occurred before instrumental records. |
doi_str_mv | 10.1029/2008GL033539 |
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A significant linear correlation was found between winter δ18Ocoral and SST measured at Ishigaki Port (SSTI), which suggests that the winter data from this coral sample is a good proxy for reconstructing past climate change. Furthermore, the winter instrumental SSTI shifted from being related to the East Asian Winter Monsoon to being dependent on the El Niño/Southern Oscillation in response to the 1988/1989 climate regime shift. 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Since this shift is also captured by the winter δ18Ocoral values, this 180‐year coral core record may provide insight into past climate regime shifts that occurred before instrumental records.</description><subject>climate regime shift</subject><subject>coral skeletal oxygen isotope ratio</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Marine</subject><subject>sea surface temperature</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><recordid>eNp9kc9uEzEQxlcIJELhxgP4Aqcu8Z_dtc0tipJQKWoRLXC0vN7ZxHTXDrajksfiwgvwYrhsVXHiMvNJ8_s-jWaK4jXB7wimck4xFpstZqxm8kkxI7KqSoExf1rMMJZZU948L17E-A1jzDAjs-LXSseEFtFqh0bvovcOJY9WA7q0v3_6-bU_pj0Eh66iscOgk_XuPVqguLd9QjbDe0B31iUIyAx21AmQ79FFnu_0rc1i0K5D2hg_HrQ7Wbf7ayFSiHkuEgXY2RGmwHPU6ggdyktYF1M4juCSHtB9hPEhqwC5d_Fl8azXQ4RXD_2s-Lxe3Sw_lNurzcVysS1NJUhdNh1pKykoMExM2wna8oZQQhvDu45ywgTvSSeZgKbGnJCeETC87XWLuwrqjp0Vb6fcQ_DfjxCTGm00kA_hwB-jIpLhStYig-cTaIKPMUCvDiFfI5wUwer-Oerf52T8zUOujkYPfdDO2PjoobiWjLMqc3Ti7uwAp_9mqs2nLa2qus6mcjLZmODHo0mHW9Vwxmv19XKj2M2X6_V6ydRH9geC0a3D</recordid><startdate>200807</startdate><enddate>200807</enddate><creator>Tsunoda, Tomoaki</creator><creator>Kawahata, Hodaka</creator><creator>Suzuki, Atsushi</creator><creator>Minoshima, Kayo</creator><creator>Shikazono, Naotatsu</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>200807</creationdate><title>East Asian monsoon to El Niño/Southern Oscillation: A shift in the winter climate of Ishigaki Island accompanying the 1988/1989 regime shift, based on instrumental and coral records</title><author>Tsunoda, Tomoaki ; Kawahata, Hodaka ; Suzuki, Atsushi ; Minoshima, Kayo ; Shikazono, Naotatsu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4815-6d1b4982e301cbd82b7612126c7dd271387f1d938e650711f31ec7bfab0d4e5d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2008</creationdate><topic>climate regime shift</topic><topic>coral skeletal oxygen isotope ratio</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Marine</topic><topic>sea surface temperature</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Tsunoda, Tomoaki</creatorcontrib><creatorcontrib>Kawahata, Hodaka</creatorcontrib><creatorcontrib>Suzuki, Atsushi</creatorcontrib><creatorcontrib>Minoshima, Kayo</creatorcontrib><creatorcontrib>Shikazono, Naotatsu</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Tsunoda, Tomoaki</au><au>Kawahata, Hodaka</au><au>Suzuki, Atsushi</au><au>Minoshima, Kayo</au><au>Shikazono, Naotatsu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>East Asian monsoon to El Niño/Southern Oscillation: A shift in the winter climate of Ishigaki Island accompanying the 1988/1989 regime shift, based on instrumental and coral records</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2008-07</date><risdate>2008</risdate><volume>35</volume><issue>13</issue><epage>n/a</epage><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>The relationship between the coral skeletal oxygen isotope ratio (δ18Ocoral) of a coral core (Porites sp.), which was collected from the inshore area of Ishigaki Island, Japan (24°N, 124°E) and represents 180 years of continuous growth, and sea surface temperature (SST) was examined for the last 30 years. A significant linear correlation was found between winter δ18Ocoral and SST measured at Ishigaki Port (SSTI), which suggests that the winter data from this coral sample is a good proxy for reconstructing past climate change. Furthermore, the winter instrumental SSTI shifted from being related to the East Asian Winter Monsoon to being dependent on the El Niño/Southern Oscillation in response to the 1988/1989 climate regime shift. Since this shift is also captured by the winter δ18Ocoral values, this 180‐year coral core record may provide insight into past climate regime shifts that occurred before instrumental records.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2008GL033539</doi><tpages>5</tpages><oa>free_for_read</oa></addata></record> |
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subjects | climate regime shift coral skeletal oxygen isotope ratio Earth sciences Earth, ocean, space Exact sciences and technology Marine sea surface temperature |
title | East Asian monsoon to El Niño/Southern Oscillation: A shift in the winter climate of Ishigaki Island accompanying the 1988/1989 regime shift, based on instrumental and coral records |
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