Coupling of Indo-Pacific climate variability over the last millennium
The Indian Ocean Dipole (IOD) affects climate and rainfall across the world, and most severely in nations surrounding the Indian Ocean 1 – 4 . The frequency and intensity of positive IOD events increased during the twentieth century 5 and may continue to intensify in a warming world 6 . However, con...
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creator | Abram, Nerilie J. Wright, Nicky M. Ellis, Bethany Dixon, Bronwyn C. Wurtzel, Jennifer B. England, Matthew H. Ummenhofer, Caroline C. Philibosian, Belle Cahyarini, Sri Yudawati Yu, Tsai-Luen Shen, Chuan-Chou Cheng, Hai Edwards, R. Lawrence Heslop, David |
description | The Indian Ocean Dipole (IOD) affects climate and rainfall across the world, and most severely in nations surrounding the Indian Ocean
1
–
4
. The frequency and intensity of positive IOD events increased during the twentieth century
5
and may continue to intensify in a warming world
6
. However, confidence in predictions of future IOD change is limited by known biases in IOD models
7
and the lack of information on natural IOD variability before anthropogenic climate change. Here we use precisely dated and highly resolved coral records from the eastern equatorial Indian Ocean, where the signature of IOD variability is strong and unambiguous, to produce a semi-continuous reconstruction of IOD variability that covers five centuries of the last millennium. Our reconstruction demonstrates that extreme positive IOD events were rare before 1960. However, the most extreme event on record (1997) is not unprecedented, because at least one event that was approximately 27 to 42 per cent larger occurred naturally during the seventeenth century. We further show that a persistent, tight coupling existed between the variability of the IOD and the El Niño/Southern Oscillation during the last millennium. Indo-Pacific coupling was characterized by weak interannual variability before approximately 1590, which probably altered teleconnection patterns, and by anomalously strong variability during the seventeenth century, which was associated with societal upheaval in tropical Asia. A tendency towards clustering of positive IOD events is evident in our reconstruction, which—together with the identification of extreme IOD variability and persistent tropical Indo-Pacific climate coupling—may have implications for improving seasonal and decadal predictions and managing the climate risks of future IOD variability.
Coral records indicate that the variability of the Indian Ocean Dipole over the last millennium is strongly coupled to variability in the El Niño/Southern Oscillation and that recent extremes are unusual but not unprecedented. |
doi_str_mv | 10.1038/s41586-020-2084-4 |
format | Article |
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1
–
4
. The frequency and intensity of positive IOD events increased during the twentieth century
5
and may continue to intensify in a warming world
6
. However, confidence in predictions of future IOD change is limited by known biases in IOD models
7
and the lack of information on natural IOD variability before anthropogenic climate change. Here we use precisely dated and highly resolved coral records from the eastern equatorial Indian Ocean, where the signature of IOD variability is strong and unambiguous, to produce a semi-continuous reconstruction of IOD variability that covers five centuries of the last millennium. Our reconstruction demonstrates that extreme positive IOD events were rare before 1960. However, the most extreme event on record (1997) is not unprecedented, because at least one event that was approximately 27 to 42 per cent larger occurred naturally during the seventeenth century. We further show that a persistent, tight coupling existed between the variability of the IOD and the El Niño/Southern Oscillation during the last millennium. Indo-Pacific coupling was characterized by weak interannual variability before approximately 1590, which probably altered teleconnection patterns, and by anomalously strong variability during the seventeenth century, which was associated with societal upheaval in tropical Asia. A tendency towards clustering of positive IOD events is evident in our reconstruction, which—together with the identification of extreme IOD variability and persistent tropical Indo-Pacific climate coupling—may have implications for improving seasonal and decadal predictions and managing the climate risks of future IOD variability.
Coral records indicate that the variability of the Indian Ocean Dipole over the last millennium is strongly coupled to variability in the El Niño/Southern Oscillation and that recent extremes are unusual but not unprecedented.</description><identifier>ISSN: 0028-0836</identifier><identifier>EISSN: 1476-4687</identifier><identifier>DOI: 10.1038/s41586-020-2084-4</identifier><identifier>PMID: 32188937</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>704/106/413 ; 704/106/694 ; Analysis ; Animals ; Anthozoa - metabolism ; Climate Change - statistics & numerical data ; Datasets as Topic ; El Nino-Southern Oscillation ; Fossils ; History, 15th Century ; History, 16th Century ; History, 17th Century ; History, 18th Century ; History, 19th Century ; History, 20th Century ; History, 21st Century ; History, Medieval ; Humanities and Social Sciences ; Indian Ocean ; Indonesia ; Islands ; Models, Theoretical ; multidisciplinary ; Ocean-atmosphere interaction ; Oxygen Isotopes ; Pacific Ocean ; Rain ; Science ; Science (multidisciplinary) ; Seasons ; Southern oscillation ; Tropical Climate</subject><ispartof>Nature (London), 2020-03, Vol.579 (7799), p.385-392</ispartof><rights>The Author(s), under exclusive licence to Springer Nature Limited 2020. corrected publication 2022</rights><rights>COPYRIGHT 2020 Nature Publishing Group</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a611t-515a000e1a2a4c580581b295027733900d3bde48a0c6f5507aad43d0e7600c83</citedby><cites>FETCH-LOGICAL-a611t-515a000e1a2a4c580581b295027733900d3bde48a0c6f5507aad43d0e7600c83</cites><orcidid>0000-0001-9696-2930 ; 0000-0002-4662-1115 ; 0000-0002-9163-3967 ; 0000-0002-5600-3193 ; 0000-0003-1246-2344</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1038/s41586-020-2084-4$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1038/s41586-020-2084-4$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/32188937$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Abram, Nerilie J.</creatorcontrib><creatorcontrib>Wright, Nicky M.</creatorcontrib><creatorcontrib>Ellis, Bethany</creatorcontrib><creatorcontrib>Dixon, Bronwyn C.</creatorcontrib><creatorcontrib>Wurtzel, Jennifer B.</creatorcontrib><creatorcontrib>England, Matthew H.</creatorcontrib><creatorcontrib>Ummenhofer, Caroline C.</creatorcontrib><creatorcontrib>Philibosian, Belle</creatorcontrib><creatorcontrib>Cahyarini, Sri Yudawati</creatorcontrib><creatorcontrib>Yu, Tsai-Luen</creatorcontrib><creatorcontrib>Shen, Chuan-Chou</creatorcontrib><creatorcontrib>Cheng, Hai</creatorcontrib><creatorcontrib>Edwards, R. Lawrence</creatorcontrib><creatorcontrib>Heslop, David</creatorcontrib><title>Coupling of Indo-Pacific climate variability over the last millennium</title><title>Nature (London)</title><addtitle>Nature</addtitle><addtitle>Nature</addtitle><description>The Indian Ocean Dipole (IOD) affects climate and rainfall across the world, and most severely in nations surrounding the Indian Ocean
1
–
4
. The frequency and intensity of positive IOD events increased during the twentieth century
5
and may continue to intensify in a warming world
6
. However, confidence in predictions of future IOD change is limited by known biases in IOD models
7
and the lack of information on natural IOD variability before anthropogenic climate change. Here we use precisely dated and highly resolved coral records from the eastern equatorial Indian Ocean, where the signature of IOD variability is strong and unambiguous, to produce a semi-continuous reconstruction of IOD variability that covers five centuries of the last millennium. Our reconstruction demonstrates that extreme positive IOD events were rare before 1960. However, the most extreme event on record (1997) is not unprecedented, because at least one event that was approximately 27 to 42 per cent larger occurred naturally during the seventeenth century. We further show that a persistent, tight coupling existed between the variability of the IOD and the El Niño/Southern Oscillation during the last millennium. Indo-Pacific coupling was characterized by weak interannual variability before approximately 1590, which probably altered teleconnection patterns, and by anomalously strong variability during the seventeenth century, which was associated with societal upheaval in tropical Asia. A tendency towards clustering of positive IOD events is evident in our reconstruction, which—together with the identification of extreme IOD variability and persistent tropical Indo-Pacific climate coupling—may have implications for improving seasonal and decadal predictions and managing the climate risks of future IOD variability.
Coral records indicate that the variability of the Indian Ocean Dipole over the last millennium is strongly coupled to variability in the El Niño/Southern Oscillation and that recent extremes are unusual but not unprecedented.</description><subject>704/106/413</subject><subject>704/106/694</subject><subject>Analysis</subject><subject>Animals</subject><subject>Anthozoa - metabolism</subject><subject>Climate Change - statistics & numerical data</subject><subject>Datasets as Topic</subject><subject>El Nino-Southern Oscillation</subject><subject>Fossils</subject><subject>History, 15th Century</subject><subject>History, 16th Century</subject><subject>History, 17th Century</subject><subject>History, 18th Century</subject><subject>History, 19th Century</subject><subject>History, 20th Century</subject><subject>History, 21st Century</subject><subject>History, Medieval</subject><subject>Humanities and Social Sciences</subject><subject>Indian Ocean</subject><subject>Indonesia</subject><subject>Islands</subject><subject>Models, Theoretical</subject><subject>multidisciplinary</subject><subject>Ocean-atmosphere interaction</subject><subject>Oxygen Isotopes</subject><subject>Pacific Ocean</subject><subject>Rain</subject><subject>Science</subject><subject>Science (multidisciplinary)</subject><subject>Seasons</subject><subject>Southern oscillation</subject><subject>Tropical Climate</subject><issn>0028-0836</issn><issn>1476-4687</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNp9kctKAzEUhoMoWi8P4EYGXYlETyaXSZdl8FIQFS24DGkmUyNzqclMsW_vlFGxoK7O4nz_z-F8CB0SOCdA5UVghEuBIQYcg2SYbaABYYnATMhkEw0AYolBUrGDdkN4BQBOEraNdmhMpBzSZIAu07qdF66aRXUejausxg_auNyZyBSu1I2NFto7PXWFa5ZRvbA-al5sVOjQRKUrCltVri330Vaui2APPucemlxdTtIbfHt_PU5Ht1gLQhrMCdfdEZboWDPDJXBJpvGQQ5wklA4BMjrNLJMajMg5h0TrjNEMbCIAjKR76KSvnenCKlfldeO1KV0waiRE1wJsyDrq-BfKzN2b-gmdrkGmrhr73sx0G4IaPz2uF579zY4mz-ndOk162vg6BG9zNffdJ_1SEVArbarXpjptaqVNrTJHfWbeTkubfSe-PHVA3AOhW1Uz69Vr3fqq-_U_rR9sw51g</recordid><startdate>20200301</startdate><enddate>20200301</enddate><creator>Abram, Nerilie J.</creator><creator>Wright, Nicky M.</creator><creator>Ellis, Bethany</creator><creator>Dixon, Bronwyn C.</creator><creator>Wurtzel, Jennifer B.</creator><creator>England, Matthew H.</creator><creator>Ummenhofer, Caroline C.</creator><creator>Philibosian, Belle</creator><creator>Cahyarini, Sri Yudawati</creator><creator>Yu, Tsai-Luen</creator><creator>Shen, Chuan-Chou</creator><creator>Cheng, Hai</creator><creator>Edwards, R. 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Lawrence</creatorcontrib><creatorcontrib>Heslop, David</creatorcontrib><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>Gale In Context: Middle School</collection><jtitle>Nature (London)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Abram, Nerilie J.</au><au>Wright, Nicky M.</au><au>Ellis, Bethany</au><au>Dixon, Bronwyn C.</au><au>Wurtzel, Jennifer B.</au><au>England, Matthew H.</au><au>Ummenhofer, Caroline C.</au><au>Philibosian, Belle</au><au>Cahyarini, Sri Yudawati</au><au>Yu, Tsai-Luen</au><au>Shen, Chuan-Chou</au><au>Cheng, Hai</au><au>Edwards, R. Lawrence</au><au>Heslop, David</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Coupling of Indo-Pacific climate variability over the last millennium</atitle><jtitle>Nature (London)</jtitle><stitle>Nature</stitle><addtitle>Nature</addtitle><date>2020-03-01</date><risdate>2020</risdate><volume>579</volume><issue>7799</issue><spage>385</spage><epage>392</epage><pages>385-392</pages><issn>0028-0836</issn><eissn>1476-4687</eissn><abstract>The Indian Ocean Dipole (IOD) affects climate and rainfall across the world, and most severely in nations surrounding the Indian Ocean
1
–
4
. The frequency and intensity of positive IOD events increased during the twentieth century
5
and may continue to intensify in a warming world
6
. However, confidence in predictions of future IOD change is limited by known biases in IOD models
7
and the lack of information on natural IOD variability before anthropogenic climate change. Here we use precisely dated and highly resolved coral records from the eastern equatorial Indian Ocean, where the signature of IOD variability is strong and unambiguous, to produce a semi-continuous reconstruction of IOD variability that covers five centuries of the last millennium. Our reconstruction demonstrates that extreme positive IOD events were rare before 1960. However, the most extreme event on record (1997) is not unprecedented, because at least one event that was approximately 27 to 42 per cent larger occurred naturally during the seventeenth century. We further show that a persistent, tight coupling existed between the variability of the IOD and the El Niño/Southern Oscillation during the last millennium. Indo-Pacific coupling was characterized by weak interannual variability before approximately 1590, which probably altered teleconnection patterns, and by anomalously strong variability during the seventeenth century, which was associated with societal upheaval in tropical Asia. A tendency towards clustering of positive IOD events is evident in our reconstruction, which—together with the identification of extreme IOD variability and persistent tropical Indo-Pacific climate coupling—may have implications for improving seasonal and decadal predictions and managing the climate risks of future IOD variability.
Coral records indicate that the variability of the Indian Ocean Dipole over the last millennium is strongly coupled to variability in the El Niño/Southern Oscillation and that recent extremes are unusual but not unprecedented.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><pmid>32188937</pmid><doi>10.1038/s41586-020-2084-4</doi><tpages>8</tpages><orcidid>https://orcid.org/0000-0001-9696-2930</orcidid><orcidid>https://orcid.org/0000-0002-4662-1115</orcidid><orcidid>https://orcid.org/0000-0002-9163-3967</orcidid><orcidid>https://orcid.org/0000-0002-5600-3193</orcidid><orcidid>https://orcid.org/0000-0003-1246-2344</orcidid></addata></record> |
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subjects | 704/106/413 704/106/694 Analysis Animals Anthozoa - metabolism Climate Change - statistics & numerical data Datasets as Topic El Nino-Southern Oscillation Fossils History, 15th Century History, 16th Century History, 17th Century History, 18th Century History, 19th Century History, 20th Century History, 21st Century History, Medieval Humanities and Social Sciences Indian Ocean Indonesia Islands Models, Theoretical multidisciplinary Ocean-atmosphere interaction Oxygen Isotopes Pacific Ocean Rain Science Science (multidisciplinary) Seasons Southern oscillation Tropical Climate |
title | Coupling of Indo-Pacific climate variability over the last millennium |
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