The Northwest Pacific corals unravel the NPGO/Victoria Mode-related temperature back to the 19th century | 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 The Northwest Pacific corals unravel the NPGO/Victoria Mode-related temperature back to the 19 th century Saori Ito, Takaaki K. Watanabe, Atsuko Yamazaki, Chuan-Chou Shen, and 2 more This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-3861020/v3 This work is licensed under a CC BY 4.0 License Status: Posted Version 3 posted You are reading this latest preprint version Show more versions Abstract Atmospheric and oceanic phenomena in the Pacific Ocean, such as the North Pacific Gyre Oscillation (NPGO) and the Victoria Mode (VM), have significant implications for global climate variability through their linkage with temperature variability in the Central Pacific (CP). The NPGO and VM manifest as sea surface height and basin-wide sea surface temperature anomaly patterns, respectively, in the North Pacific. Although recent studies have drawn attention to their connections with surface temperature anomalies in the CP, their historical interactions remain poorly understood due to limited instrumental observations. Here, we present a long-term reconstruction of NPGO/VM-related temperature variability based on a coral Sr/Ca temperature proxy from the Northwest Pacific, covering the period from 1798 to 2014 Common Era. This reconstruction contributes to a better spatiotemporal understanding of historical interactions among NPGO, VM, and surface temperature anomalies in the CP over the past two centuries. The coral-inferred temperature record closely aligns with surface temperature variability in the CP, indicating the extra-tropical propagation of NPGO/VM-related temperature variations from the CP via an ocean-atmosphere bridge. Our reconstruction identifies pronounced negative-NPGO/cool-temperature phases in the late 1840s and during the 1860s–1900s, and a positive-NPGO/warm-temperature phase during the 2000s–2010s. We also find a significant correlation between surface temperature anomalies in the CP and interannual to decadal NPGO/VM variability throughout the past 200 years. This relationship lasted from the early 20th century until 2014, with the exception of the period from the 1970s to the 1990s, and strengthened from the 2000s onward. Given the strong linkage between the NPGO and the surface temperature anomalies in the CP, as well as the projected increase in CP-centred climate variability under future warming scenarios, the prominence of the NPGO in the North Pacific and beyond is expected to intensify. Full Text Cite Share Download PDF Status: Posted Version 3 posted You are reading this latest preprint version Show more versions 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. As a division of Research Square Company, we’re committed to making research communication faster, fairer, and more useful. We do this by developing innovative software and high quality services for the global research community. Our growing team is made up of researchers and industry professionals working together to solve the most critical problems facing scientific publishing. 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-3861020","acceptedTermsAndConditions":true,"allowDirectSubmit":true,"archivedVersions":[],"articleType":"Research Article","associatedPublications":[],"authors":[{"id":490405673,"identity":"551cc040-556e-4c7a-a018-e6f456605744","order_by":0,"name":"Saori Ito","email":"data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAAZAAAAAyAQMAAABI0h/eAAAABlBMVEX///8AAABVwtN+AAAACXBIWXMAAA7EAAAOxAGVKw4bAAABE0lEQVRIie2QsUrEMBjH/0Fol2LXFDzuFT7oIujDNBR0ERFcOh0JB95y0LWHg6/gG9gS0MUHqLgoB7o4ZHDo4GBaPW/KnaNgfiGQhO/H9/0DeDx/lQwcCJU0/SWwq8YZmNyicESNqtYKbVEsHDxj1dc5sHuDMp7pW/OE/UmcLJV6hz7dRSBqQxiVDoXuj/KqHyy5FGq6B31uB6ubipAuHG0IJ+mQhR7FbMmhxcX4VeqIIK5rx2Dl27fy0KjpoCCU+sMqNw4F7apLy5QygxLUGn0XV5b2JUdGPFnMbRbQca9kzZx4WjkHyzXrikkch3fPqisOxJUMUtMVh6PSEX/1CQM7Ef088U31a1j3uzqPx+P5Z3wCuBdYRe8doAkAAAAASUVORK5CYII=","orcid":"","institution":"Kiel University","correspondingAuthor":true,"prefix":"","firstName":"Saori","middleName":"","lastName":"Ito","suffix":""},{"id":490405674,"identity":"7fd0165d-9e0a-4c56-8685-5e48a97e5e53","order_by":1,"name":"Takaaki K. Watanabe","email":"","orcid":"","institution":"Kiel University","correspondingAuthor":false,"prefix":"","firstName":"Takaaki","middleName":"K.","lastName":"Watanabe","suffix":""},{"id":490405675,"identity":"cef684d2-3a1e-4729-b1a9-607f564bb17b","order_by":2,"name":"Atsuko Yamazaki","email":"","orcid":"","institution":"Nagoya University","correspondingAuthor":false,"prefix":"","firstName":"Atsuko","middleName":"","lastName":"Yamazaki","suffix":""},{"id":490405676,"identity":"7d7d26a0-d1a2-4f7e-a32e-c27d93bb5531","order_by":3,"name":"Chuan-Chou Shen","email":"","orcid":"","institution":"National Taiwan University","correspondingAuthor":false,"prefix":"","firstName":"Chuan-Chou","middleName":"","lastName":"Shen","suffix":""},{"id":490405677,"identity":"99ab0928-146f-4084-9adb-f0ede825ef63","order_by":4,"name":"Taro Komagoe","email":"","orcid":"","institution":"KIKAI Institute for Coral Reef Sciences","correspondingAuthor":false,"prefix":"","firstName":"Taro","middleName":"","lastName":"Komagoe","suffix":""},{"id":490405678,"identity":"5f65b1e5-9b21-473e-a200-7d9311d48e46","order_by":5,"name":"Tsuyoshi Watanabe","email":"","orcid":"","institution":"Hokkaido University","correspondingAuthor":false,"prefix":"","firstName":"Tsuyoshi","middleName":"","lastName":"Watanabe","suffix":""}],"badges":[],"createdAt":"2024-01-13 18:59:12","currentVersionCode":3,"declarations":{"humanSubjects":false,"vertebrateSubjects":false,"conflictsOfInterestStatement":false,"humanSubjectEthicalGuidelines":false,"humanSubjectConsent":false,"humanSubjectClinicalTrial":false,"humanSubjectCaseReport":false,"vertebrateSubjectEthicalGuidelines":false},"doi":"10.21203/rs.3.rs-3861020/v3","doiUrl":"https://doi.org/10.21203/rs.3.rs-3861020/v3","draftVersion":[],"editorialEvents":[],"editorialNote":"","failedWorkflow":false,"files":[{"id":90052521,"identity":"c9dca3a5-aca7-4a1f-b84d-7934a4cb9703","added_by":"auto","created_at":"2025-08-27 21:56:56","extension":"pdf","order_by":1,"title":"","display":"","copyAsset":false,"role":"manuscript-pdf","size":6275593,"visible":true,"origin":"","legend":"","description":"","filename":"egusphere20254054manuscriptversion1.pdf","url":"https://assets-eu.researchsquare.com/files/rs-3861020/v3_covered_c767ea5c-54ef-4c16-ab1b-bded30ca4ba2.pdf"}],"financialInterests":"","formattedTitle":"\u003cp\u003eThe Northwest Pacific corals unravel the NPGO/Victoria Mode-related temperature back to the 19\u003csup\u003eth\u003c/sup\u003e century\u003c/p\u003e","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":"
[email protected]","identity":"researchsquare","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":true,"externalIdentity":"","sideBox":"","snPcode":"","submissionUrl":"/submission","title":"Research Square","twitterHandle":"researchsquare","acdcEnabled":true,"dfaEnabled":false,"editorialSystem":"","reportingPortfolio":"","inReviewEnabled":false,"inReviewRevisionsEnabled":true},"keywords":"","lastPublishedDoi":"10.21203/rs.3.rs-3861020/v3","lastPublishedDoiUrl":"https://doi.org/10.21203/rs.3.rs-3861020/v3","license":{"name":"CC BY 4.0","url":"https://creativecommons.org/licenses/by/4.0/"},"manuscriptAbstract":"\u003cp\u003eAtmospheric and oceanic phenomena in the Pacific Ocean, such as the North Pacific Gyre Oscillation (NPGO) and the Victoria Mode (VM), have significant implications for global climate variability through their linkage with temperature variability in the Central Pacific (CP). The NPGO and VM manifest as sea surface height and basin-wide sea surface temperature anomaly patterns, respectively, in the North Pacific. Although recent studies have drawn attention to their connections with surface temperature anomalies in the CP, their historical interactions remain poorly understood due to limited instrumental observations. Here, we present a long-term reconstruction of NPGO/VM-related temperature variability based on a coral Sr/Ca temperature proxy from the Northwest Pacific, covering the period from 1798 to 2014 Common Era. This reconstruction contributes to a better spatiotemporal understanding of historical interactions among NPGO, VM, and surface temperature anomalies in the CP over the past two centuries. The coral-inferred temperature record closely aligns with surface temperature variability in the CP, indicating the extra-tropical propagation of NPGO/VM-related temperature variations from the CP via an ocean-atmosphere bridge. Our reconstruction identifies pronounced negative-NPGO/cool-temperature phases in the late 1840s and during the 1860s–1900s, and a positive-NPGO/warm-temperature phase during the 2000s–2010s. We also find a significant correlation between surface temperature anomalies in the CP and interannual to decadal NPGO/VM variability throughout the past 200 years. This relationship lasted from the early 20th century until 2014, with the exception of the period from the 1970s to the 1990s, and strengthened from the 2000s onward. Given the strong linkage between the NPGO and the surface temperature anomalies in the CP, as well as the projected increase in CP-centred climate variability under future warming scenarios, the prominence of the NPGO in the North Pacific and beyond is expected to intensify.\u003c/p\u003e","manuscriptTitle":"The Northwest Pacific corals unravel the NPGO/Victoria Mode-related temperature back to the 19th century","msid":"","msnumber":"","nonDraftVersions":[{"code":3,"date":"2025-08-26 18:33:42","doi":"10.21203/rs.3.rs-3861020/v3","editorialEvents":[{"type":"communityComments","content":0}],"status":"published","journal":{"display":true,"email":"
[email protected]","identity":"researchsquare","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":true,"externalIdentity":"","sideBox":"","snPcode":"","submissionUrl":"/submission","title":"Research Square","twitterHandle":"researchsquare","acdcEnabled":true,"dfaEnabled":false,"editorialSystem":"","reportingPortfolio":"","inReviewEnabled":false,"inReviewRevisionsEnabled":true}},{"code":2,"date":"2025-08-12 17:53:03","doi":"10.21203/rs.3.rs-3861020/v2","editorialEvents":[{"type":"communityComments","content":0}],"status":"published","journal":{"display":true,"email":"
[email protected]","identity":"researchsquare","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":true,"externalIdentity":"","sideBox":"","snPcode":"","submissionUrl":"/submission","title":"Research Square","twitterHandle":"researchsquare","acdcEnabled":true,"dfaEnabled":false,"editorialSystem":"","reportingPortfolio":"","inReviewEnabled":false,"inReviewRevisionsEnabled":true}},{"code":1,"date":"2024-01-18 19:27:28","doi":"10.21203/rs.3.rs-3861020/v1","editorialEvents":[{"type":"communityComments","content":0}],"status":"published","journal":{"display":true,"email":"
[email protected]","identity":"researchsquare","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":true,"externalIdentity":"","sideBox":"","snPcode":"","submissionUrl":"/submission","title":"Research Square","twitterHandle":"researchsquare","acdcEnabled":true,"dfaEnabled":false,"editorialSystem":"","reportingPortfolio":"","inReviewEnabled":false,"inReviewRevisionsEnabled":true}}],"origin":"","ownerIdentity":"c271b89a-dea2-4113-920c-38072ad4b6bf","owner":[],"postedDate":"August 26th, 2025","published":true,"recentEditorialEvents":[],"rejectedJournal":[],"revision":"","amendment":"","status":"posted","subjectAreas":[],"tags":[],"updatedAt":"2025-08-27T21:51:58+00:00","versionOfRecord":[],"versionCreatedAt":"2025-08-26 18:33:42","video":"","vorDoi":"","vorDoiUrl":"","workflowStages":[]},"version":"v3","identity":"rs-3861020","journalConfig":"researchsquare"},"__N_SSP":true},"page":"/article/[identity]/[[...version]]","query":{"redirect":"/article/rs-3861020","identity":"rs-3861020","version":["v3"]},"buildId":"8U1c8b4HqxoKbykW_rLl7","isFallback":false,"isExperimentalCompile":false,"dynamicIds":[84888],"gssp":true,"scriptLoader":[]}
Text is read by the "Ask this paper" AI Q&A widget below.
Extraction quality varies by source — PMC NXML preserves structure
cleanly, OA-HTML may include some navigation residue, and OA-PDF can
have broken hyphenation. The publisher copy
(via DOI)
is the canonical version.