East Asian hydroclimate modulated by the position of the westerlies during Termination I
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- Hongbin Zhang
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China.
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- Michael L. Griffiths
- Department of Environmental Science, William Paterson University, Wayne, NJ 07470, USA.
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- John C. H. Chiang
- Department of Geography and Berkeley Atmospheric Sciences Center, University of California, Berkeley, CA 94720, USA.
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- Wenwen Kong
- Department of Geography and Berkeley Atmospheric Sciences Center, University of California, Berkeley, CA 94720, USA.
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- Shitou Wu
- Department of Geochemistry, Faculty of Geoscience and Geography, Georg-August University Goettingen, Goettingen 37077, Germany.
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- Alyssa Atwood
- Department of Geography and Berkeley Atmospheric Sciences Center, University of California, Berkeley, CA 94720, USA.
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- Junhua Huang
- State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China.
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- Hai Cheng
- Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an, 710049, China.
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- Youfeng Ning
- Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an, 710049, China.
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- Shucheng Xie
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China.
書誌事項
- 公開日
- 2018-11-02
- DOI
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- 10.1126/science.aat9393
- 公開者
- American Association for the Advancement of Science (AAAS)
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説明
<jats:title>East Asian monsoon mysteries</jats:title> <jats:p> What exactly does the oxygen isotopic composition of speleothems tell us about the East Asian monsoon? They provide magnificent, detailed records of hydroclimate, but precisely what aspects of hydroclimate they record is unclear. Zhang <jats:italic>et al.</jats:italic> present data from two speleothems from central eastern China for the period from 21,000 to 10,000 years ago and suggest that the cause of the oxygen isotopic variability that they observe is more complex than simple changes in monsoon strength or intensity (see the Perspective by McGee). Alternatively, this variation may reflect the lengths of various phases of the monsoon and the regional heterogeneity of the East Asian hydroclimate. </jats:p> <jats:p> <jats:italic>Science</jats:italic> , this issue p. <jats:related-article xmlns:xlink="http://www.w3.org/1999/xlink" ext-link-type="doi" issue="6414" page="580" related-article-type="in-this-issue" vol="362" xlink:href="10.1126/science.aat9393">580</jats:related-article> ; see also p. <jats:related-article xmlns:xlink="http://www.w3.org/1999/xlink" ext-link-type="doi" issue="6414" page="518" related-article-type="in-this-issue" vol="362" xlink:href="10.1126/science.aav5280">518</jats:related-article> </jats:p>
収録刊行物
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- Science
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Science 362 (6414), 580-583, 2018-11-02
American Association for the Advancement of Science (AAAS)
