Projected changes in the global precipitation area by CMIP6 models

preprint OA: closed
Full text JSON View at publisher
Full text 14,080 characters · extracted from preprint-html · click to expand
Projected changes in the global precipitation area by CMIP6 models | 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 Article Projected changes in the global precipitation area by CMIP6 models Andreas Dobler, Rasmus Benestad, Cristian Lussana, Oskar Landgren This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-4546090/v1 This work is licensed under a CC BY 4.0 License Status: Published Journal Publication published 08 Oct, 2024 Read the published version in npj Climate and Atmospheric Science → Version 1 posted 11 You are reading this latest preprint version Abstract Reanalysis and satellite data indicate a decreasing precipitation area in recent decades, affecting local water resources and precipitation intensities. We have used CMIP6 simulations to test the hypothesis of a shrinking precipitation area in a warming climate. Our analyses reveal that SSP5-8.5 projections show a robust decrease in the precipitation area towards the end of the 21st century. The decrease is most pronounced between 50 °S and 50 °N. We find a poleward shift of precipitation, increasing the daily precipitation area in the Arctic from 18 % to 28 %. The new findings support the observed relationship, although to a lesser extent than earlier found for reanalysis and satellite data. An explanation is provided by the expansion of low relative humidity zones in the lower-to-mid troposphere poleward of the subtropics. The expansion locally decreases the occurrence of precipitation and pushes precipitation events poleward, ultimately leading to a reduced global precipitation area. Earth and environmental sciences/Climate sciences/Atmospheric science/Atmospheric dynamics Earth and environmental sciences/Climate sciences/Climate change/Projection and prediction Earth and environmental sciences/Climate sciences/Climate change/Climate-change impacts Earth and environmental sciences/Climate sciences/Climate change/Climate and Earth system modelling Global hydrological cycle global warming rainfall patterns precipitation intensity CMIP6 Full Text Additional Declarations (Not answered) Supplementary Files CMIP6rainareaSI.pdf Cite Share Download PDF Status: Published Journal Publication published 08 Oct, 2024 Read the published version in npj Climate and Atmospheric Science → Version 1 posted Editorial decision: revise 22 Jul, 2024 Review # 1 received at journal 11 Jul, 2024 Review # 2 received at journal 10 Jul, 2024 Reviewer # 3 agreed at journal 19 Jun, 2024 Reviewer # 2 agreed at journal 18 Jun, 2024 Reviewer # 1 agreed at journal 17 Jun, 2024 Reviewers invited by journal 17 Jun, 2024 Editor assigned by journal 16 Jun, 2024 Submission checks completed at journal 14 Jun, 2024 First submitted to journal 12 Jun, 2024 Unknown event 10 Jun, 2024 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. 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-4546090","acceptedTermsAndConditions":true,"allowDirectSubmit":false,"archivedVersions":[],"articleType":"Article","associatedPublications":[],"authors":[{"id":315479344,"identity":"3675ec1c-bbfe-409c-b0b6-20b8e25f4218","order_by":0,"name":"Andreas Dobler","email":"data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAAZAAAAAyAQMAAABI0h/eAAAABlBMVEX///8AAABVwtN+AAAACXBIWXMAAA7EAAAOxAGVKw4bAAAAsElEQVRIiWNgGAWjYHACAxDB2E+6lpkNDIwNpGnZcIBYLfyzm7d9+FBTJ7v52uHjDxh32BDWInHnWPHMGccOG2+7nZbYwHgmjQhrbuQYM/OwHUjcdjvHsIGx7TBhHfIgLX/+1SVunp3/kTgtBiAtjG3MiRukcxiJ02J4I62YsbfvsPGM22mGMxLbiPCL3I3kzQw/vtXJ9s9OfvDhYxsRIYYKEkjVMApGwSgYBaMAOwAAQ6E+o1MzyPAAAAAASUVORK5CYII=","orcid":"https://orcid.org/0000-0001-9490-0840","institution":"Norwegian Meteorological Institute","correspondingAuthor":true,"prefix":"","firstName":"Andreas","middleName":"","lastName":"Dobler","suffix":""},{"id":315479345,"identity":"f32f5404-d1fb-41c9-9f0a-3699cad74e9d","order_by":1,"name":"Rasmus Benestad","email":"","orcid":"","institution":"Norwegian Meteorological Institute","correspondingAuthor":false,"prefix":"","firstName":"Rasmus","middleName":"","lastName":"Benestad","suffix":""},{"id":315479346,"identity":"cf32aa80-ffae-4512-9b8c-d37476e3fb3b","order_by":2,"name":"Cristian Lussana","email":"","orcid":"","institution":"Norwegian Meteorological Institute","correspondingAuthor":false,"prefix":"","firstName":"Cristian","middleName":"","lastName":"Lussana","suffix":""},{"id":315479347,"identity":"971369ed-13f8-4e3e-8e69-2c201492d343","order_by":3,"name":"Oskar Landgren","email":"","orcid":"","institution":"Norwegian Meteorological Institute","correspondingAuthor":false,"prefix":"","firstName":"Oskar","middleName":"","lastName":"Landgren","suffix":""}],"badges":[],"createdAt":"2024-06-07 12:25:55","currentVersionCode":1,"declarations":"","doi":"10.21203/rs.3.rs-4546090/v1","doiUrl":"https://doi.org/10.21203/rs.3.rs-4546090/v1","draftVersion":[],"editorialEvents":[{"content":"https://doi.org/10.1038/s41612-024-00794-z","type":"published","date":"2024-10-08T04:00:00+00:00"}],"editorialNote":"","failedWorkflow":false,"files":[{"id":66242664,"identity":"167ba416-71c4-40c6-be5f-bc30d06116f7","added_by":"auto","created_at":"2024-10-09 07:05:54","extension":"pdf","order_by":1,"title":"","display":"","copyAsset":false,"role":"manuscript-pdf","size":3801533,"visible":true,"origin":"","legend":"","description":"","filename":"CMIP6rainarea.pdf","url":"https://assets-eu.researchsquare.com/files/rs-4546090/v1_covered_858c205a-7626-4599-b60b-95b65476f586.pdf"},{"id":59550221,"identity":"556c1971-398e-4679-8ca5-fd18f6407bcd","added_by":"auto","created_at":"2024-07-03 06:10:59","extension":"pdf","order_by":1,"title":"","display":"","copyAsset":false,"role":"supplement","size":9204037,"visible":true,"origin":"","legend":"\u003cp\u003e\u003cbr\u003e\u003c/p\u003e","description":"","filename":"CMIP6rainareaSI.pdf","url":"https://assets-eu.researchsquare.com/files/rs-4546090/v1/194cccbaa904eeac483e961c.pdf"}],"financialInterests":"(Not answered)","formattedTitle":"Projected changes in the global precipitation area by CMIP6 models","fulltext":[],"fulltextSource":"","fullText":"","funders":[],"hasAdminPriorityOnWorkflow":false,"hasManuscriptDocX":false,"hasOptedInToPreprint":true,"hasPassedJournalQc":"","hasAnyPriority":false,"hideJournal":false,"highlight":"","institution":"","isAcceptedByJournal":true,"isAuthorSuppliedPdf":true,"isDeskRejected":"","isHiddenFromSearch":false,"isInQc":false,"isInWorkflow":false,"isPdf":true,"isPdfUpToDate":true,"isWithdrawnOrRetracted":false,"journal":{"display":true,"email":"[email protected]","identity":"npj-climate-and-atmospheric-science","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":false,"externalIdentity":"npjclimatsci","sideBox":"Learn more about [npj Climate and Atmospheric Science](http://www.nature.com/npjclimatsci/)","snPcode":"41612","submissionUrl":"https://submission.springernature.com/new-submission/41612/3","title":"npj Climate and Atmospheric Science","twitterHandle":"","acdcEnabled":true,"dfaEnabled":true,"editorialSystem":"stoa","reportingPortfolio":"NPJ","inReviewEnabled":true,"inReviewRevisionsEnabled":true},"keywords":"Global hydrological cycle, global warming, rainfall patterns, precipitation intensity, CMIP6","lastPublishedDoi":"10.21203/rs.3.rs-4546090/v1","lastPublishedDoiUrl":"https://doi.org/10.21203/rs.3.rs-4546090/v1","license":{"name":"CC BY 4.0","url":"https://creativecommons.org/licenses/by/4.0/"},"manuscriptAbstract":"Reanalysis and satellite data indicate a decreasing precipitation area in recent decades, affecting local water resources and precipitation intensities. We have used CMIP6 simulations to test the hypothesis of a shrinking precipitation area in a warming climate. Our analyses reveal that SSP5-8.5 projections show a robust decrease in the precipitation area towards the end of the 21st century. The decrease is most pronounced between 50 °S and 50 °N. We find a poleward shift of precipitation, increasing the daily precipitation area in the Arctic from 18 % to 28 %.\r\nThe new findings support the observed relationship, although to a lesser extent than earlier found for reanalysis and satellite data. An explanation is provided by the expansion of low relative humidity zones in the lower-to-mid troposphere poleward of the subtropics. The expansion locally decreases the occurrence of precipitation and pushes precipitation events poleward, ultimately leading to a reduced global precipitation area.","manuscriptTitle":"Projected changes in the global precipitation area by CMIP6 models","msid":"","msnumber":"","nonDraftVersions":[{"code":1,"date":"2024-07-03 06:10:54","doi":"10.21203/rs.3.rs-4546090/v1","editorialEvents":[{"type":"communityComments","content":0},{"type":"decision","content":"revise","date":"2024-07-22T13:22:39+00:00","index":"","fulltext":""},{"type":"editorInvitedReview","content":"This content is not available.","date":"2024-07-11T08:40:54+00:00","index":1,"fulltext":"This content is not available."},{"type":"editorInvitedReview","content":"This content is not available.","date":"2024-07-10T04:35:52+00:00","index":2,"fulltext":"This content is not available."},{"type":"reviewerAgreed","content":"This content is not available.","date":"2024-06-19T06:34:20+00:00","index":3,"fulltext":"This content is not available."},{"type":"reviewerAgreed","content":"This content is not available.","date":"2024-06-18T05:52:11+00:00","index":2,"fulltext":"This content is not available."},{"type":"reviewerAgreed","content":"This content is not available.","date":"2024-06-17T18:01:53+00:00","index":1,"fulltext":"This content is not available."},{"type":"reviewersInvited","content":"","date":"2024-06-17T14:35:53+00:00","index":"","fulltext":""},{"type":"editorAssigned","content":"","date":"2024-06-16T10:23:26+00:00","index":"","fulltext":""},{"type":"checksComplete","content":"","date":"2024-06-14T15:14:33+00:00","index":"","fulltext":""},{"type":"submitted","content":"npj Climate and Atmospheric Science","date":"2024-06-12T14:27:52+00:00","index":"","fulltext":""},{"type":"checksFailed","content":"","date":"2024-06-10T14:58:32+00:00","index":"","fulltext":""}],"status":"published","journal":{"display":true,"email":"[email protected]","identity":"npj-climate-and-atmospheric-science","isNatureJournal":false,"hasQc":true,"allowDirectSubmit":false,"externalIdentity":"npjclimatsci","sideBox":"Learn more about [npj Climate and Atmospheric Science](http://www.nature.com/npjclimatsci/)","snPcode":"41612","submissionUrl":"https://submission.springernature.com/new-submission/41612/3","title":"npj Climate and Atmospheric Science","twitterHandle":"","acdcEnabled":true,"dfaEnabled":true,"editorialSystem":"stoa","reportingPortfolio":"NPJ","inReviewEnabled":true,"inReviewRevisionsEnabled":true}}],"origin":"","ownerIdentity":"58c55a72-31f8-4c50-ac66-b84ea0b0a305","owner":[],"postedDate":"July 3rd, 2024","published":true,"recentEditorialEvents":[],"rejectedJournal":[],"revision":"","amendment":"","status":"published-in-journal","subjectAreas":[{"id":33359949,"name":"Earth and environmental sciences/Climate sciences/Atmospheric science/Atmospheric dynamics"},{"id":33359950,"name":"Earth and environmental sciences/Climate sciences/Climate change/Projection and prediction"},{"id":33359951,"name":"Earth and environmental sciences/Climate sciences/Climate change/Climate-change impacts"},{"id":33359952,"name":"Earth and environmental sciences/Climate sciences/Climate change/Climate and Earth system modelling"}],"tags":[],"updatedAt":"2024-10-09T07:05:44+00:00","versionOfRecord":{"articleIdentity":"rs-4546090","link":"https://doi.org/10.1038/s41612-024-00794-z","journal":{"identity":"npj-climate-and-atmospheric-science","isVorOnly":false,"title":"npj Climate and Atmospheric Science"},"publishedOn":"2024-10-08 04:00:00","publishedOnDateReadable":"October 8th, 2024"},"versionCreatedAt":"2024-07-03 06:10:54","video":"","vorDoi":"10.1038/s41612-024-00794-z","vorDoiUrl":"https://doi.org/10.1038/s41612-024-00794-z","workflowStages":[]},"version":"v1","identity":"rs-4546090","journalConfig":"researchsquare"},"__N_SSP":true},"page":"/article/[identity]/[[...version]]","query":{"redirect":"/article/rs-4546090","identity":"rs-4546090","version":["v1"]},"buildId":"qtupq5eGEP_6zYnWcrvyt","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.

My notes (saved in your browser only)

Ask this paper AI returns verbatim quotes from the full text · source: preprint-html

Answers must be backed by verbatim quotes from this paper's full text. Hallucinated quotes are dropped automatically; if no verbatim passage answers the question, we say so. How this works

Citation neighborhood (no data yet)

We don't have any in-corpus citations linked to this paper yet. This is a recent paper (2024) — citers typically take a year or two to land, and the OpenAlex reference graph may still be filling in.

Source provenance

europepmc
last seen: 2026-05-20T01:45:00.602351+00:00