{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361981470375355264.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1073/pnas.1610930114"}},{"identifier":{"@type":"URI","@value":"http://www.pnas.org/syndication/doi/10.1073/pnas.1610930114"}},{"identifier":{"@type":"URI","@value":"https://pnas.org/doi/pdf/10.1073/pnas.1610930114"}}],"dc:title":[{"@value":"Holocene ENSO-related cyclic storms recorded by magnetic minerals in speleothems of central China"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Significance</jats:title>\n          <jats:p>High-resolution reconstructions of storm history and storms’ underlying mechanisms in inland areas are critical but limited by a paucity of suitable paleoproxies. Here we use soil-derived magnetic minerals preserved in a stalagmite as a new paleohydrological proxy. This proxy enables us to rebuild decadal resolution storm records in the eastern Asian monsoon area since 8.6 ky. Variance of storms in central China was found to exhibit close correlation with El Niño−Southern Oscillation activity at millennial and centennial time scales, and also occur on a significant 500-y cycle related to periodic solar activity. These findings shed light on the forecasting of future floods and improve our understanding of the potential mechanism of strong precipitation in monsoon regions.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981470375355267","@type":"Researcher","foaf:name":[{"@value":"Zongmin Zhu"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China;"},{"@value":"Institute for Rock Magnetism, University of Minnesota, Minneapolis, MN 55455;"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470375355268","@type":"Researcher","foaf:name":[{"@value":"Joshua M. Feinberg"}],"jpcoar:affiliationName":[{"@value":"Institute for Rock Magnetism, University of Minnesota, Minneapolis, MN 55455;"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470375355266","@type":"Researcher","foaf:name":[{"@value":"Shucheng Xie"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China;"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470375355264","@type":"Researcher","foaf:name":[{"@value":"Mark D. Bourne"}],"jpcoar:affiliationName":[{"@value":"Institute for Rock Magnetism, University of Minnesota, Minneapolis, MN 55455;"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470375355136","@type":"Researcher","foaf:name":[{"@value":"Chunju Huang"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China;"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470375355265","@type":"Researcher","foaf:name":[{"@value":"Chaoyong Hu"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China;"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981470375355269","@type":"Researcher","foaf:name":[{"@value":"Hai Cheng"}],"jpcoar:affiliationName":[{"@value":"Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710049, China"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00278424"},{"@type":"EISSN","@value":"10916490"}],"prism:publicationName":[{"@value":"Proceedings of the National Academy of Sciences"}],"dc:publisher":[{"@value":"Proceedings of the National Academy of Sciences"}],"prism:publicationDate":"2017-01-17","prism:volume":"114","prism:number":"5","prism:startingPage":"852","prism:endingPage":"857"},"reviewed":"false","dc:rights":["http://www.pnas.org/site/misc/userlicense.xhtml"],"url":[{"@id":"http://www.pnas.org/syndication/doi/10.1073/pnas.1610930114"},{"@id":"https://pnas.org/doi/pdf/10.1073/pnas.1610930114"}],"createdAt":"2017-01-18","modifiedAt":"2022-04-13","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360025430649073024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Obtaining High‐Resolution Magnetic Records From Speleothems Using Magnetic Microscopy"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417125247104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High spatial resolution magnetic mapping using ultra-high sensitivity scanning SQUID microscopy on a speleothem from the Kingdom of Tonga, southern Pacific"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1073/pnas.1610930114"},{"@type":"CROSSREF","@value":"10.1029/2024gc011594_references_DOI_WH6yjVYfQykarhZW59BuxtSaDfJ"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01401-8_references_DOI_WH6yjVYfQykarhZW59BuxtSaDfJ"}]}