Impacts of Antarctic heatwaves amplified by climate change through water vapor and cloud feedbacks

preprint OA: gold CC-BY-4.0
📄 Open PDF Full text JSON View at publisher

Abstract

Abstract Antarctic heatwaves driven by atmospheric rivers are emerging as high-impact extremes, yet the role of climate change in amplifying such events remains uncertain. Here we investigate the climate change contribution to the March 2022 East Antarctic heatwave using pseudo-global warming experiments with the snow-atmospheric coupled model CRYOWRF. By comparing present-day and preindustrial storylines, we identify that under current climate, cloud and water-vapor radiation feedbacks non-linearly amplify near-surface warming by up to 25% relative to preindustrial conditions. These feedbacks are likely underrepresented in global climate models due to their use of hydrostatic dynamics, and poor cloud representation over coarse resolutions. Future warming further intensifies this amplification, particularly in coastal regions where firn air content is depleted, meltwater percolates, and ice lenses thicken. Such melting conditions threaten to accelerate surface mass loss and destabilize the fringing ice shelves. Our results reveal a key amplification pathway for Antarctic extremes, with potentially far-reaching implications for ice-sheet stability.
Full text 12,603 characters · extracted from preprint-html · click to expand
Impacts of Antarctic heatwaves amplified by climate change through water vapor and cloud feedbacks | 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 Impacts of Antarctic heatwaves amplified by climate change through water vapor and cloud feedbacks Sergi González-Herrero, Pranab Deb, Shihan Li, Daniel Argueso, and 4 more This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-7712953/v1 This work is licensed under a CC BY 4.0 License Status: Under Review Version 1 posted You are reading this latest preprint version Abstract Antarctic heatwaves driven by atmospheric rivers are emerging as high-impact extremes, yet the role of climate change in amplifying such events remains uncertain. Here we investigate the climate change contribution to the March 2022 East Antarctic heatwave using pseudo-global warming experiments with the snow-atmospheric coupled model CRYOWRF. By comparing present-day and preindustrial storylines, we identify that under current climate, cloud and water-vapor radiation feedbacks non-linearly amplify near-surface warming by up to 25% relative to preindustrial conditions. These feedbacks are likely underrepresented in global climate models due to their use of hydrostatic dynamics, and poor cloud representation over coarse resolutions. Future warming further intensifies this amplification, particularly in coastal regions where firn air content is depleted, meltwater percolates, and ice lenses thicken. Such melting conditions threaten to accelerate surface mass loss and destabilize the fringing ice shelves. Our results reveal a key amplification pathway for Antarctic extremes, with potentially far-reaching implications for ice-sheet stability. Earth and environmental sciences/Climate sciences/Climate change/Attribution Earth and environmental sciences/Climate sciences/Climate change/Climate-change impacts Earth and environmental sciences/Climate sciences/Cryospheric science Full Text Additional Declarations There is NO Competing Interest. Supplementary Files PGWMarch202220250923Supplementary.docx Supplementary information Cite Share Download PDF Status: Under Review 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. 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-7712953","acceptedTermsAndConditions":true,"allowDirectSubmit":false,"archivedVersions":[],"articleType":"Article","associatedPublications":[],"authors":[{"id":523782423,"identity":"df4f5a01-3f4d-4281-9de8-ed6c5f746d78","order_by":0,"name":"Sergi González-Herrero","email":"data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAAZAAAAAyAQMAAABI0h/eAAAABlBMVEX///8AAABVwtN+AAAACXBIWXMAAA7EAAAOxAGVKw4bAAAA80lEQVRIie3PMWvCQBjG8ec4eF2OugYE/QovCNVCqV/lQiGzYweVgKBL3d36Few3uHCQLKGuBZdAQRxTXBwyNKUWnC6Ohd5/eZf7wXOAz/dX0z9HGOAeN9JAXktQkwhE+gryW01sM+ktVx+HAtPuoG0LU1bbERHEcewgnGe3Q42sfxennKzVLlwQZGftIkFErJGGmyRmq4Kdpl5MUrmGvezPxLZKW/Hb9zA3wTvJQmMSblLFFtqIRRPhPCJoNn3O1Th5No/1X8S84xy2TOXn6WnW5W32Wpyqh1GbZHJ0DgMoQD3pIhG7ASBLYNb0yOfz+f5zX2LUScHEe8GgAAAAAElFTkSuQmCC","orcid":"","institution":"WSL Institut for Snow and Avalanche Research SLF","correspondingAuthor":true,"prefix":"","firstName":"Sergi","middleName":"","lastName":"González-Herrero","suffix":""},{"id":523782424,"identity":"c5627855-4d06-4b67-a153-9e1dc480bef2","order_by":1,"name":"Pranab Deb","email":"","orcid":"","institution":"Indian Institute of Technology","correspondingAuthor":false,"prefix":"","firstName":"Pranab","middleName":"","lastName":"Deb","suffix":""},{"id":523782425,"identity":"eddd2229-d287-4f56-822e-c652f5eae4a6","order_by":2,"name":"Shihan Li","email":"","orcid":"","institution":"University of Sheffield","correspondingAuthor":false,"prefix":"","firstName":"Shihan","middleName":"","lastName":"Li","suffix":""},{"id":523782426,"identity":"7b508627-d3e6-4a8d-872a-9be0e7f14f78","order_by":3,"name":"Daniel Argueso","email":"","orcid":"https://orcid.org/0000-0002-4792-162X","institution":"UNSW","correspondingAuthor":false,"prefix":"","firstName":"Daniel","middleName":"","lastName":"Argueso","suffix":""},{"id":523782427,"identity":"38b0f68a-456f-435b-9734-9bf0cf534180","order_by":4,"name":"Rainette Engbers","email":"","orcid":"","institution":"École Polytechnique Fédérale de Lausanne (EPFL)","correspondingAuthor":false,"prefix":"","firstName":"Rainette","middleName":"","lastName":"Engbers","suffix":""},{"id":523782428,"identity":"7f1dfbf4-3d38-4b18-a324-6e76246730f5","order_by":5,"name":"Michael Matějka","email":"","orcid":"https://orcid.org/0000-0003-1108-7474","institution":"Masarykova University","correspondingAuthor":false,"prefix":"","firstName":"Michael","middleName":"","lastName":"Matějka","suffix":""},{"id":523782429,"identity":"2656c08d-f26a-4626-ae3b-44f2a48ba1da","order_by":6,"name":"Nander Wever","email":"","orcid":"","institution":"WSL Institute for the Snow and Avalanche Research (SLF)","correspondingAuthor":false,"prefix":"","firstName":"Nander","middleName":"","lastName":"Wever","suffix":""},{"id":523782430,"identity":"22e76a4b-a943-4245-ba79-f881d97b4a6f","order_by":7,"name":"Michael Lehning","email":"","orcid":"","institution":"WSL Institute for the Snow and Avalanche Research (SLF)","correspondingAuthor":false,"prefix":"","firstName":"Michael","middleName":"","lastName":"Lehning","suffix":""}],"badges":[],"createdAt":"2025-09-25 12:35:08","currentVersionCode":1,"declarations":"","doi":"10.21203/rs.3.rs-7712953/v1","doiUrl":"https://doi.org/10.21203/rs.3.rs-7712953/v1","draftVersion":[],"editorialEvents":[],"editorialNote":"","failedWorkflow":false,"files":[{"id":95528911,"identity":"486b6cca-f13f-4f3e-9154-a8a64059587b","added_by":"auto","created_at":"2025-11-10 10:16:36","extension":"pdf","order_by":1,"title":"","display":"","copyAsset":false,"role":"manuscript-pdf","size":1814501,"visible":true,"origin":"","legend":"","description":"","filename":"PGWMarch202220250923.pdf","url":"https://assets-eu.researchsquare.com/files/rs-7712953/v1_covered_992531f9-88fa-4a4d-9191-db80491a9825.pdf"},{"id":95497510,"identity":"da26ae50-87a1-4062-bfb5-242c13599063","added_by":"auto","created_at":"2025-11-10 04:51:30","extension":"docx","order_by":1,"title":"","display":"","copyAsset":false,"role":"supplement","size":3930103,"visible":true,"origin":"","legend":"Supplementary information","description":"","filename":"PGWMarch202220250923Supplementary.docx","url":"https://assets-eu.researchsquare.com/files/rs-7712953/v1/0a0a3f0f8278473fe730902b.docx"}],"financialInterests":"There is \u003cb\u003eNO\u003c/b\u003e Competing Interest.","formattedTitle":"Impacts of Antarctic heatwaves amplified by climate change through water vapor and cloud feedbacks","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":"nature-portfolio","isNatureJournal":true,"hasQc":false,"allowDirectSubmit":false,"externalIdentity":"","sideBox":"","snPcode":"","submissionUrl":"","title":"Nature Portfolio","twitterHandle":"","acdcEnabled":false,"dfaEnabled":false,"editorialSystem":"ejp","reportingPortfolio":"","inReviewEnabled":true,"inReviewRevisionsEnabled":false},"keywords":"","lastPublishedDoi":"10.21203/rs.3.rs-7712953/v1","lastPublishedDoiUrl":"https://doi.org/10.21203/rs.3.rs-7712953/v1","license":{"name":"CC BY 4.0","url":"https://creativecommons.org/licenses/by/4.0/"},"manuscriptAbstract":"\u003cp\u003eAntarctic heatwaves driven by atmospheric rivers are emerging as high-impact extremes, yet the role of climate change in amplifying such events remains uncertain. Here we investigate the climate change contribution to the March 2022 East Antarctic heatwave using pseudo-global warming experiments with the snow-atmospheric coupled model CRYOWRF. By comparing present-day and preindustrial storylines, we identify that under current climate, cloud and water-vapor radiation feedbacks non-linearly amplify near-surface warming by up to 25% relative to preindustrial conditions. These feedbacks are likely underrepresented in global climate models due to their use of hydrostatic dynamics, and poor cloud representation over coarse resolutions. Future warming further intensifies this amplification, particularly in coastal regions where firn air content is depleted, meltwater percolates, and ice lenses thicken. Such melting conditions threaten to accelerate surface mass loss and destabilize the fringing ice shelves. Our results reveal a key amplification pathway for Antarctic extremes, with potentially far-reaching implications for ice-sheet stability.\u003c/p\u003e","manuscriptTitle":"Impacts of Antarctic heatwaves amplified by climate change through water vapor and cloud feedbacks","msid":"","msnumber":"","nonDraftVersions":[{"code":1,"date":"2025-11-10 04:51:25","doi":"10.21203/rs.3.rs-7712953/v1","editorialEvents":[],"status":"published","journal":{"display":true,"email":"[email protected]","identity":"communications-earth-and-environment","isNatureJournal":true,"hasQc":false,"allowDirectSubmit":false,"externalIdentity":"commsenv","sideBox":"Learn more about [Communications Earth and Environment](https://www.nature.com/commsenv/)","snPcode":"","submissionUrl":"","title":"Communications Earth \u0026 Environment","twitterHandle":"","acdcEnabled":true,"dfaEnabled":true,"editorialSystem":"ejp","reportingPortfolio":"Communications Series","inReviewEnabled":true,"inReviewRevisionsEnabled":false}}],"origin":"","ownerIdentity":"de8f2f04-63f1-45e4-940a-5b651a1e35e7","owner":[],"postedDate":"November 10th, 2025","published":true,"recentEditorialEvents":[],"rejectedJournal":[],"revision":"","amendment":"","status":"under-review","subjectAreas":[{"id":55671350,"name":"Earth and environmental sciences/Climate sciences/Climate change/Attribution"},{"id":55671351,"name":"Earth and environmental sciences/Climate sciences/Climate change/Climate-change impacts"},{"id":55671352,"name":"Earth and environmental sciences/Climate sciences/Cryospheric science"}],"tags":[],"updatedAt":"2025-11-10T04:51:25+00:00","versionOfRecord":[],"versionCreatedAt":"2025-11-10 04:51:25","video":"","vorDoi":"","vorDoiUrl":"","workflowStages":[]},"version":"v1","identity":"rs-7712953","journalConfig":"researchsquare"},"__N_SSP":true},"page":"/article/[identity]/[[...version]]","query":{"redirect":"/article/rs-7712953","identity":"rs-7712953","version":["v1"]},"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.

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 (2025) — 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
unpaywall
last seen: 2026-05-21T05:10:58.409756+00:00
License: CC-BY-4.0