East Asian hydroclimate modulated by the position of the westerlies during Termination I
Speleothem oxygen isotope records have revolutionized our understanding of the paleo East Asian monsoon, yet there is fundamental disagreement on what they represent in terms of the hydroclimate changes. We report a multiproxy speleothem record of monsoon evolution during the last deglaciation from...
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| Veröffentlicht in: | Science (American Association for the Advancement of Science) 2018-11, Vol.362 (6414), p.580-583 |
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| creator | Zhang, Hongbin Griffiths, Michael L Chiang, John C H Kong, Wenwen Wu, Shitou Atwood, Alyssa Huang, Junhua Cheng, Hai Ning, Youfeng Xie, Shucheng |
| description | Speleothem oxygen isotope records have revolutionized our understanding of the paleo East Asian monsoon, yet there is fundamental disagreement on what they represent in terms of the hydroclimate changes. We report a multiproxy speleothem record of monsoon evolution during the last deglaciation from the middle Yangtze region, which indicates a wetter central eastern China during North Atlantic cooling episodes, despite the oxygen isotopic record suggesting a weaker monsoon. We show that this apparent contradiction can be resolved if the changes are interpreted as a lengthening of the Meiyu rains and shortened post-Meiyu stage, in accordance with a recent hypothesis. Model simulations support this interpretation and further reveal the role of the westerlies in communicating the North Atlantic influence to the East Asian climate. |
| doi_str_mv | 10.1126/science.aat9393 |
| format | Article |
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We report a multiproxy speleothem record of monsoon evolution during the last deglaciation from the middle Yangtze region, which indicates a wetter central eastern China during North Atlantic cooling episodes, despite the oxygen isotopic record suggesting a weaker monsoon. We show that this apparent contradiction can be resolved if the changes are interpreted as a lengthening of the Meiyu rains and shortened post-Meiyu stage, in accordance with a recent hypothesis. Model simulations support this interpretation and further reveal the role of the westerlies in communicating the North Atlantic influence to the East Asian climate.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.aat9393</identifier><identifier>PMID: 30385577</identifier><language>eng</language><publisher>United States: The American Association for the Advancement of Science</publisher><subject>Communication ; Computer simulation ; Deglaciation ; Heterogeneity ; Hydroclimate ; Isotopes ; Monsoons ; Ocean currents ; Oxygen ; Oxygen isotopes ; Wind</subject><ispartof>Science (American Association for the Advancement of Science), 2018-11, Vol.362 (6414), p.580-583</ispartof><rights>Copyright © 2018 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. 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| identifier | ISSN: 0036-8075 |
| ispartof | Science (American Association for the Advancement of Science), 2018-11, Vol.362 (6414), p.580-583 |
| issn | 0036-8075 1095-9203 |
| language | eng |
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| source | JSTOR Archive Collection A-Z Listing; American Association for the Advancement of Science |
| subjects | Communication Computer simulation Deglaciation Heterogeneity Hydroclimate Isotopes Monsoons Ocean currents Oxygen Oxygen isotopes Wind |
| title | East Asian hydroclimate modulated by the position of the westerlies during Termination I |
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