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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Veröffentlicht in:Nature (London) 2020-03, Vol.579 (7799), p.385-392
Hauptverfasser: 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
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container_issue 7799
container_start_page 385
container_title Nature (London)
container_volume 579
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
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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. 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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. 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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. 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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. 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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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