{"@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/1364233269349348352.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/jd094id15p18409"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJD094iD15p18409"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JD094iD15p18409"}},{"identifier":{"@type":"NAID","@value":"80005023375"}}],"dc:title":[{"@value":"Forcing of late Cenozoic northern hemisphere climate by plateau uplift in southern Asia and the American west"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Geologic evidence indicates that net vertical uplift occurred on a large (kilometer) scale and at accelerating rates during the middle and late Cenozoic in plateaus of southern Asia and the American west. Based on this evidence, General Circulation Model sensitivity tests were run to isolate the unique effects of plateau uplift on climate. The experiments simulated significant climatic changes in many places, some far from the uplifted regions. The basic direction of most of these simulated responses to progressive uplift is borne out by changes found in the geologic record: winter cooling of North America, northern Europe, northern Asia, and the Arctic Ocean; summer drying of the North American west coast, the Eurasian interior, and the Mediterranean; winter drying of the North American northern plains and the interior of Asia; and changes over the North Atlantic Ocean conducive to increased formation of deep water. The modeled changes result from increased orographic diversion of westerly winds, from cyclonic and anticyclonic surface flow induced by summer heating and winter cooling of the uplifted plateaus, and from the intensification of vertical circulation cells in the atmosphere caused by exchanges of mass between the summer‐heated (and winter‐cooled) plateaus and the mid‐latitude oceans. Disagreements between the geologic record and the model simulations in Alaska and the Southern Rockies and plains may be related mainly to the lack of narrow mountain barriers in the model orography. Taken together, the observed regional trends comprise much of the pattern of “late Cenozoic climatic deterioration” in the northern hemisphere that culminated in the Plio‐Pleistocene ice ages. The success of the uplift sensitivity experiment in simulating the correct pattern and sign of most of the observed regional climatic trends points to uplift as an important forcing function of late Cenozoic climatic change in the northern hemisphere at time scales longer than orbital variations; however, the modest amplitude of the uplift‐induced cooling simulated at high latitudes indicates a probable need for additional climatic forcing.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1584231876404933632","@type":"Researcher","foaf:name":[{"@value":"W. F. Ruddiman"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233269349348353","@type":"Researcher","foaf:name":[{"@value":"J. E. Kutzbach"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Atmospheres"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1989-12-20","prism:volume":"94","prism:number":"D15","prism:startingPage":"18409","prism:endingPage":"18427"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJD094iD15p18409"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JD094iD15p18409"}],"createdAt":"2008-02-06","modifiedAt":"2023-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360865815671408256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variability of the Indonesian Throughflow and Australian monsoon across the mid Pleistocene transition (IODP 363, Site U1483)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855565730816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Diatom and Radiolarian Biostratigraphy in the Vicinity of the 2011 Tohoku Earthquake Source Fault in\n                    <scp>IODP</scp>\n                    Hole 343‐\n                    <scp>C0019E</scp>\n                    of\n                    <scp>JFAST</scp>"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204309889536","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Extinction of Siwalik fossil apes: a review based on a new fossil tooth and on palaeoecological and palaeoclimatological evidence"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204550679168","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sr isotope ratios of acid-leached loess residues from Luochuan, China: A tracer of continental weathering intensity over the past 2.5 Ma."}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238286208","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evolution and variability of Asian Monsoon"},{"@language":"ja","@value":"アジア・モンスーンの進化と変動"},{"@value":"アジア・モンスーンの進化と変動--そのヒマラヤ-チベット隆起とのリンケージ"},{"@language":"ja-Kana","@value":"アジア モンスーン ノ シンカ ト ヘンドウ ソノ ヒマラヤ チベット リュウキ ト ノ リンケージ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206502063616","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effects of Large-Scale Mountains on Surface Climate. A Coupled Ocean-Atmosphere General Circulation Model Study."},{"@value":"Effects of large-scale mountains on surface climate—A coupled ocean-atmosphere general circulation model study"}]},{"@id":"https://cir.nii.ac.jp/crid/1521980705798276992","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"Environmental magnetic record of the fluvial sediments from the Tianzhu borehole in Beijing for the last 800 ka"},{"@language":"ja-Kana","@value":"Environmental magnetic record of the fluvial sediments from the Tianzhu borehole in Beijing for the last 800 ka"}]},{"@id":"https://cir.nii.ac.jp/crid/1524232505445169024","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phylogeography of the Rice Spittle Bug (Callitettix versicolor) Implies Two Long-Term Mountain Barriers in South China"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151841908060032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution and variability of the Asian monsoon and its potential linkage with uplift of the Himalaya and Tibetan Plateau"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/jd094id15p18409"},{"@type":"CIA","@value":"80005023375"},{"@type":"CROSSREF","@value":"10.2151/jmsj.80.1165_references_DOI_VUGbEZyknRvxUmBmF0GkQqteyl9"},{"@type":"CROSSREF","@value":"10.1186/s40645-016-0080-y_references_DOI_VUGbEZyknRvxUmBmF0GkQqteyl9"},{"@type":"CROSSREF","@value":"10.5575/geosoc.111.668_references_DOI_VUGbEZyknRvxUmBmF0GkQqteyl9"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2023.118437_references_DOI_VUGbEZyknRvxUmBmF0GkQqteyl9"},{"@type":"CROSSREF","@value":"10.1111/iar.70009_references_DOI_VUGbEZyknRvxUmBmF0GkQqteyl9"},{"@type":"CROSSREF","@value":"10.2108/zs160042_references_DOI_VUGbEZyknRvxUmBmF0GkQqteyl9"}]}