A 900y Annual Temperature Reconstruction for the Southeastern Tibetan Plateau from Tree Ring Width of Juniperus saltuaria | Research Square window.SnipcartSettings = { analytics: { enabled: false } }; (function() { var accessVector = localStorage.getItem('access_vector') || ''; window.dataLayer = window.dataLayer || []; if (accessVector) { window.dataLayer.push({ user: { profile: { profileInfo: { snid: accessVector } } } }); } })(); (function(w,d,s,l,i){w[l]=w[l]||[];w[l].push({'gtm.start':new Date().getTime(),event:'gtm.js'});var f=d.getElementsByTagName(s)[0],j=d.createElement(s),dl=l!='dataLayer'?'&l='+l:'';j.async=true;j.src='https://www.googletagmanager.com/gtm.js?id='+i+dl;f.parentNode.insertBefore(j,f);})(window,document,'script','dataLayer','GTM-K279D39R'); Browse Preprints In Review Journals COVID-19 Preprints AJE Video Bytes Research Tools Research Promotion AJE Professional Editing AJE Rubriq About Preprint Platform In Review Editorial Policies Our Team Advisory Board Help Center Sign In Submit a Preprint Cite Share Download PDF Research Article A 900y Annual Temperature Reconstruction for the Southeastern Tibetan Plateau from Tree Ring Width of Juniperus saltuaria Shanshan Xu, Zhiyuan Shang, Chaogang Zheng, Zhigang Zhang, Xinggong Kong, and 1 more This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-4142317/v1 This work is licensed under a CC BY 4.0 License Status: Posted Version 1 posted You are reading this latest preprint version Abstract Two annually resolved and absolutely dated Juniperus saltuaria (JS) tree ring width chronologies from the Haizi mountain, southeastern TP were reported in here. We sampled two sites in different landscapes, one is located at the forest line at ca. 4200 m above sea level beside an incised valley, and the other at the plateau surface, ca. 4500 m in elevation. Comparisons of statistical parameters between two sites and their tree ring index correlation coefficient with meteorologic data of DaoCheng shows that the latter site exhibits higher value than the former one. These indicate that those trees growing along the valley side may be more susceptible to local environment, and those on the plateau surface can provide reliable record for regional climate. Based on the latter chronology, a 903a long annual mean temperature (Tmean) series (1115-2017 CE) was reconstructed. It is the longest width chronology reconstructed by JS at present. The entire sequence shows consistent warm-cold patterns with other temperature reconstructions of the TP, Asia, and Northern Hemisphere. The warmest (coldest) period occurred at 1998-2017 CE (1115-1145 CE), respectively. There was no doubt that temperature raised sharply since the end of the 20th century. In addition, the sequence demonstrates multi-decadal, decadal and inter-decadal variations, further multi-taper method reveals dominant periodicities are 147, 36, 18, 7 and 2-2.6a, likely been affected by the Atlantic Multidecadal Oscillation and solar activity. The forcing of volcanic eruptions resulted to subsequent 1-3 years temperature drops. Tree ring Southeastern Tibetan Plateau Climate reconstruction Mean annual temperature Last millennium Full Text Supplementary Files chronology.xlsx Cite Share Download PDF Status: Posted Version 1 posted You are reading this latest preprint version Research Square lets you share your work early, gain feedback from the community, and start making changes to your manuscript prior to peer review in a journal. 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Also discoverable on Platform About Our Team In Review Editorial Policies Advisory Board Help Center Resources Author Services Accessibility API Access RSS feed Manage Cookie Preferences © Research Square 2026 | ISSN 2693-5015 (online) Privacy Policy Terms of Service Do Not Sell My Personal Information {"props":{"pageProps":{"initialData":{"identity":"rs-4142317","acceptedTermsAndConditions":true,"allowDirectSubmit":true,"archivedVersions":[],"articleType":"Research Article","associatedPublications":[],"authors":[{"id":288891791,"identity":"363db619-c956-4089-a3aa-f603378324d9","order_by":0,"name":"Shanshan Xu","email":"data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAAZAAAAAyAQMAAABI0h/eAAAABlBMVEX///8AAABVwtN+AAAACXBIWXMAAA7EAAAOxAGVKw4bAAAA+UlEQVRIiWNgGAWjYBACfvbG5gcJBhI89u0NDAZgoQMEtEj2HG4z+FBgI2fAc4BILQY30hskZ3xIMzaQSIAKEdLCcCCxwZjH4HDidsm3B4oL2xjk+G4kMH4uwKODseFgw2OQlp2z8xKMZ7YxGEveSGCWnoFHCzNjI8SWhts5Bsa8bQyJG24ksDHz4NHCxszYIA3WcvMMWEs9QS08bIxA7xsAvX+DB6wlwYCQFgkeRmAgG9jISfYAHcZzTsJw5pmHzdL4tNjff/74QcIfCR5+9jNmxjxlNvJ8x5MPfsanBcVfwKiUYACFIpEagKH3gGilo2AUjIJRMKIAAFMDTQkb61tlAAAAAElFTkSuQmCC","orcid":"https://orcid.org/0009-0009-7496-8982","institution":"Nanjing Normal University","correspondingAuthor":true,"prefix":"","firstName":"Shanshan","middleName":"","lastName":"Xu","suffix":""},{"id":288891792,"identity":"bc0d2d5f-771a-4a52-ae77-06027b105cbb","order_by":1,"name":"Zhiyuan Shang","email":"","orcid":"https://orcid.org/0000-0002-3478-7820","institution":"Nanjing Normal University","correspondingAuthor":false,"prefix":"","firstName":"Zhiyuan","middleName":"","lastName":"Shang","suffix":""},{"id":288891793,"identity":"6c7f85a6-88c6-4f6d-a18c-42190ec89982","order_by":2,"name":"Chaogang Zheng","email":"","orcid":"","institution":"Nanjing Normal University","correspondingAuthor":false,"prefix":"","firstName":"Chaogang","middleName":"","lastName":"Zheng","suffix":""},{"id":288891794,"identity":"d2aee406-32be-40c6-a081-87401663d0c8","order_by":3,"name":"Zhigang Zhang","email":"","orcid":"","institution":"Nanjing Normal University","correspondingAuthor":false,"prefix":"","firstName":"Zhigang","middleName":"","lastName":"Zhang","suffix":""},{"id":288891795,"identity":"0580ec42-1314-4550-b45e-644966fde7dc","order_by":4,"name":"Xinggong Kong","email":"","orcid":"","institution":"Nanjing Normal University","correspondingAuthor":false,"prefix":"","firstName":"Xinggong","middleName":"","lastName":"Kong","suffix":""},{"id":288891796,"identity":"0b743da1-a427-4af2-8a58-6792500612e4","order_by":5,"name":"Zhijun Zhao","email":"","orcid":"","institution":"Nanjing Normal University","correspondingAuthor":false,"prefix":"","firstName":"Zhijun","middleName":"","lastName":"Zhao","suffix":""}],"badges":[],"createdAt":"2024-03-21 09:28:41","currentVersionCode":1,"declarations":"","doi":"10.21203/rs.3.rs-4142317/v1","doiUrl":"https://doi.org/10.21203/rs.3.rs-4142317/v1","draftVersion":[],"editorialEvents":[],"editorialNote":"","failedWorkflow":false,"files":[{"id":56653696,"identity":"fce53aff-da91-4afd-9927-18d5a4fe2996","added_by":"auto","created_at":"2024-05-17 09:20:55","extension":"pdf","order_by":1,"title":"","display":"","copyAsset":false,"role":"manuscript-pdf","size":1493915,"visible":true,"origin":"","legend":"","description":"","filename":"manuscript.pdf","url":"https://assets-eu.researchsquare.com/files/rs-4142317/v1_covered_56b716be-317f-4815-ac46-1955c7921805.pdf"},{"id":54522630,"identity":"2b5a54b8-9ca8-4aca-a134-02a9966c8d94","added_by":"auto","created_at":"2024-04-11 18:32:58","extension":"xlsx","order_by":1,"title":"","display":"","copyAsset":false,"role":"supplement","size":40815,"visible":true,"origin":"","legend":"","description":"","filename":"chronology.xlsx","url":"https://assets-eu.researchsquare.com/files/rs-4142317/v1/cf92b9a1acdea0aded0b5dec.xlsx"}],"financialInterests":"","formattedTitle":"A 900y Annual Temperature Reconstruction for the Southeastern Tibetan Plateau from Tree Ring Width of Juniperus saltuaria","fulltext":[],"fulltextSource":"","fullText":"","funders":[],"hasAdminPriorityOnWorkflow":false,"hasManuscriptDocX":false,"hasOptedInToPreprint":true,"hasPassedJournalQc":"","hasAnyPriority":false,"hideJournal":true,"highlight":"","institution":"","isAcceptedByJournal":false,"isAuthorSuppliedPdf":true,"isDeskRejected":"","isHiddenFromSearch":false,"isInQc":false,"isInWorkflow":false,"isPdf":true,"isPdfUpToDate":true,"isWithdrawnOrRetracted":false,"journal":{"display":true,"email":"
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