Three-Dimensional Canopy Morphology and Wind Dynamics Govern Global Rainfall Interception

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

Abstract

Abstract Accurate simulation of rainfall interception is critical for understanding the global water cycle, yet most earth system models rely on simplified, leaf area index (LAI)-centric vegetation representations that neglect the three-dimensional (3D) structure of plant canopies, introducing substantial structural uncertainty. Here we introduce Feature-Constrained Deep Symbolic Regression (FC-DSR), an interpretable artificial intelligence framework that derives explicit parameterizations for canopy interception. Global analyses show that 3D canopy morphology (canopy depth and width) and wind dynamics exert stronger control on interception than LAI. The resulting morphology-based parameterizations substantially outperform conventional LAI-based approaches, increasing site-level interception loss Kling–Gupta efficiency by 0.27–0.39. Budyko-based water-balance analyses confirm the improved interception scheme, with enhanced evapotranspiration at nearly 70% of global flux sites and stronger runoff dynamics across six major river basins. Implementation of the new scheme in the CoLM land surface model improves runoff simulations for 71.5% of U.S. catchments and better reproduces discharge variability in representative sites. Global applications further reveal highly nonlinear responses of interception to changes in rainfall intensity and vegetation structure. Together, these results highlight fundamental limitations of LAI-centered models and demonstrate that explicit representation of 3D canopy architecture is critical for reliable prediction of the terrestrial water balance.
Full text 14,206 characters · extracted from preprint-html · click to expand
Three-Dimensional Canopy Morphology and Wind Dynamics Govern Global Rainfall Interception | 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 Three-Dimensional Canopy Morphology and Wind Dynamics Govern Global Rainfall Interception Qingliang Li, Xiaochun Jin, Zhongwang Wei, Cheng Zhang, Wei Shangguan, and 6 more This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-8346448/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 Accurate simulation of rainfall interception is critical for understanding the global water cycle, yet most earth system models rely on simplified, leaf area index (LAI)-centric vegetation representations that neglect the three-dimensional (3D) structure of plant canopies, introducing substantial structural uncertainty. Here we introduce Feature-Constrained Deep Symbolic Regression (FC-DSR), an interpretable artificial intelligence framework that derives explicit parameterizations for canopy interception. Global analyses show that 3D canopy morphology (canopy depth and width) and wind dynamics exert stronger control on interception than LAI. The resulting morphology-based parameterizations substantially outperform conventional LAI-based approaches, increasing site-level interception loss Kling–Gupta efficiency by 0.27–0.39. Budyko-based water-balance analyses confirm the improved interception scheme, with enhanced evapotranspiration at nearly 70% of global flux sites and stronger runoff dynamics across six major river basins. Implementation of the new scheme in the CoLM land surface model improves runoff simulations for 71.5% of U.S. catchments and better reproduces discharge variability in representative sites. Global applications further reveal highly nonlinear responses of interception to changes in rainfall intensity and vegetation structure. Together, these results highlight fundamental limitations of LAI-centered models and demonstrate that explicit representation of 3D canopy architecture is critical for reliable prediction of the terrestrial water balance. Earth and environmental sciences/Hydrology Earth and environmental sciences/Climate sciences/Hydrology Full Text Additional Declarations There is NO Competing Interest. Supplementary Files supplementary.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-8346448","acceptedTermsAndConditions":true,"allowDirectSubmit":false,"archivedVersions":[],"articleType":"Article","associatedPublications":[],"authors":[{"id":573120538,"identity":"898815ba-cfbf-42b6-a63b-be195b65839b","order_by":0,"name":"Qingliang Li","email":"data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAAZAAAAAyAQMAAABI0h/eAAAABlBMVEX///8AAABVwtN+AAAACXBIWXMAAA7EAAAOxAGVKw4bAAABA0lEQVRIiWNgGAWjYBACPmYGhgMMDBY8QDbjAyDBDxKVwKeFDaJFAqSF2QBISDYQ1AKhwGrYJIjTws688XDBLwkZ/tnt1yp+1NRJGBxgPnibh8EuD7fD2AoOz+yT4JG4c6bsZs+xw0AtbMnWPAzJxbi18Bgc5u0B+uVGTtptxoYDdQYHeMykeRgOJDYQ0iIP1FLM2AByGP83wlp4fkjwGNxIP8bM2MAM1MLDRkAL0C+8DRI8hjdymCVBfpE8zGZsOccgGacWfv7Dmz/z/LGxl7uR/vADKMT4jjc/vPGmwg6nFiAwYGBsA9E8BhA+M0QQHwDK/gHR7A/wKhsFo2AUjIKRCwCFF07RCHnnHwAAAABJRU5ErkJggg==","orcid":"","institution":"College of Computer Science and Technology, Changchun Normal University","correspondingAuthor":true,"prefix":"","firstName":"Qingliang","middleName":"","lastName":"Li","suffix":""},{"id":573120539,"identity":"d78deeef-303d-48b5-a64f-c58d669bd34e","order_by":1,"name":"Xiaochun Jin","email":"","orcid":"","institution":"College of Computer Science and Technology, Changchun Normal University","correspondingAuthor":false,"prefix":"","firstName":"Xiaochun","middleName":"","lastName":"Jin","suffix":""},{"id":573120540,"identity":"ead7a2dc-f481-4631-bed8-335a6bd0d134","order_by":2,"name":"Zhongwang Wei","email":"","orcid":"","institution":"School of Atmospheric Sciences, Sun Yat-Sen University","correspondingAuthor":false,"prefix":"","firstName":"Zhongwang","middleName":"","lastName":"Wei","suffix":""},{"id":573120541,"identity":"011696e1-fe1d-4561-8f85-6e829a0e00fa","order_by":3,"name":"Cheng Zhang","email":"","orcid":"","institution":"College of Computer Science and Technology, Jilin University","correspondingAuthor":false,"prefix":"","firstName":"Cheng","middleName":"","lastName":"Zhang","suffix":""},{"id":573120542,"identity":"8a72e361-9097-4010-8d0e-41d09ee3856d","order_by":4,"name":"Wei Shangguan","email":"","orcid":"","institution":"School of Atmospheric Sciences, Sun Yat-Sen University","correspondingAuthor":false,"prefix":"","firstName":"Wei","middleName":"","lastName":"Shangguan","suffix":""},{"id":573120543,"identity":"581bfada-b6d5-4c77-ae3e-471045e8d444","order_by":5,"name":"Jinlong Zhu","email":"","orcid":"","institution":"College of Computer Science and Technology, Changchun Normal University","correspondingAuthor":false,"prefix":"","firstName":"Jinlong","middleName":"","lastName":"Zhu","suffix":""},{"id":573120544,"identity":"1cba668c-d2f0-4c01-a11e-a191ca90ccff","order_by":6,"name":"Zijian Zhang","email":"","orcid":"","institution":"College of Computer Science and Technology, Jilin University","correspondingAuthor":false,"prefix":"","firstName":"Zijian","middleName":"","lastName":"Zhang","suffix":""},{"id":573120545,"identity":"887af617-25be-421b-8c63-e21ad5e726f6","order_by":7,"name":"Xiaoning Li","email":"","orcid":"","institution":"College of Computer Science and Technology, Changchun Normal University","correspondingAuthor":false,"prefix":"","firstName":"Xiaoning","middleName":"","lastName":"Li","suffix":""},{"id":573120546,"identity":"e22361fe-a2dd-44a8-9af4-57409da9d3ba","order_by":8,"name":"Yuguang Yan","email":"","orcid":"","institution":"College of Computer Science and Technology, Changchun Normal University","correspondingAuthor":false,"prefix":"","firstName":"Yuguang","middleName":"","lastName":"Yan","suffix":""},{"id":573120547,"identity":"74fddad2-5063-472c-8ae9-fffc57cce186","order_by":9,"name":"Jing Wang","email":"","orcid":"","institution":"College of Computer Science and Technology, Changchun Normal University","correspondingAuthor":false,"prefix":"","firstName":"Jing","middleName":"","lastName":"Wang","suffix":""},{"id":573120548,"identity":"88fe089c-4d78-4c6d-a382-917ec20d9ab2","order_by":10,"name":"Yongjiu Dai","email":"","orcid":"","institution":"School of Atmospheric Sciences, Sun Yat-Sen University","correspondingAuthor":false,"prefix":"","firstName":"Yongjiu","middleName":"","lastName":"Dai","suffix":""}],"badges":[],"createdAt":"2025-12-12 13:55:10","currentVersionCode":1,"declarations":"","doi":"10.21203/rs.3.rs-8346448/v1","doiUrl":"https://doi.org/10.21203/rs.3.rs-8346448/v1","draftVersion":[],"editorialEvents":[],"editorialNote":"","failedWorkflow":false,"files":[{"id":101751556,"identity":"f38a38f1-c327-4def-b929-fb6f9fd38965","added_by":"auto","created_at":"2026-02-03 10:21:17","extension":"pdf","order_by":1,"title":"","display":"","copyAsset":false,"role":"manuscript-pdf","size":2119461,"visible":true,"origin":"","legend":"","description":"","filename":"manuscript.pdf","url":"https://assets-eu.researchsquare.com/files/rs-8346448/v1_covered_e7b4473e-9867-413b-a9e9-6bd0bfe9400c.pdf"},{"id":101490734,"identity":"595ecd96-af4a-4ad3-95e8-976dfd9bb3e7","added_by":"auto","created_at":"2026-01-30 10:00:49","extension":"docx","order_by":1,"title":"","display":"","copyAsset":false,"role":"supplement","size":15243449,"visible":true,"origin":"","legend":"SUPPLEMENTARY INFORMATION","description":"","filename":"supplementary.docx","url":"https://assets-eu.researchsquare.com/files/rs-8346448/v1/bf346d3e0e56b22bbd7b3909.docx"}],"financialInterests":"There is \u003cb\u003eNO\u003c/b\u003e Competing Interest.","formattedTitle":"Three-Dimensional Canopy Morphology and Wind Dynamics Govern Global Rainfall Interception","fulltext":[],"fulltextSource":"","fullText":"","funders":[],"hasAdminPriorityOnWorkflow":false,"hasManuscriptDocX":false,"hasOptedInToPreprint":true,"hasPassedJournalQc":"","hasAnyPriority":false,"hideJournal":false,"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":"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-8346448/v1","lastPublishedDoiUrl":"https://doi.org/10.21203/rs.3.rs-8346448/v1","license":{"name":"CC BY 4.0","url":"https://creativecommons.org/licenses/by/4.0/"},"manuscriptAbstract":"\u003cp\u003eAccurate simulation of rainfall interception is critical for understanding the global water cycle, yet most earth system models rely on simplified, leaf area index (LAI)-centric vegetation representations that neglect the three-dimensional (3D) structure of plant canopies, introducing substantial structural uncertainty. Here we introduce Feature-Constrained Deep Symbolic Regression (FC-DSR), an interpretable artificial intelligence framework that derives explicit parameterizations for canopy interception. Global analyses show that 3D canopy morphology (canopy depth and width) and wind dynamics exert stronger control on interception than LAI. The resulting morphology-based parameterizations substantially outperform conventional LAI-based approaches, increasing site-level interception loss Kling\u0026ndash;Gupta efficiency by 0.27\u0026ndash;0.39. Budyko-based water-balance analyses confirm the improved interception scheme, with enhanced evapotranspiration at nearly 70% of global flux sites and stronger runoff dynamics across six major river basins. Implementation of the new scheme in the CoLM land surface model improves runoff simulations for 71.5% of U.S. catchments and better reproduces discharge variability in representative sites. Global applications further reveal highly nonlinear responses of interception to changes in rainfall intensity and vegetation structure. Together, these results highlight fundamental limitations of LAI-centered models and demonstrate that explicit representation of 3D canopy architecture is critical for reliable prediction of the terrestrial water balance.\u003c/p\u003e","manuscriptTitle":"Three-Dimensional Canopy Morphology and Wind Dynamics Govern Global Rainfall Interception","msid":"","msnumber":"","nonDraftVersions":[{"code":1,"date":"2026-01-30 10:00:44","doi":"10.21203/rs.3.rs-8346448/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":"a3c7850e-488a-4422-83ec-65e085bcc7b6","owner":[],"postedDate":"January 30th, 2026","published":true,"recentEditorialEvents":[],"rejectedJournal":[],"revision":"","amendment":"","status":"under-review","subjectAreas":[{"id":60974158,"name":"Earth and environmental sciences/Hydrology"},{"id":60974159,"name":"Earth and environmental sciences/Climate sciences/Hydrology"}],"tags":[],"updatedAt":"2026-01-30T10:00:44+00:00","versionOfRecord":[],"versionCreatedAt":"2026-01-30 10:00:44","video":"","vorDoi":"","vorDoiUrl":"","workflowStages":[]},"version":"v1","identity":"rs-8346448","journalConfig":"researchsquare"},"__N_SSP":true},"page":"/article/[identity]/[[...version]]","query":{"redirect":"/article/rs-8346448","identity":"rs-8346448","version":["v1"]},"buildId":"XKTyCvWXoU3ODBz1xrDgd","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 (2026) — 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: 2026-06-02T02:00:03.124865+00:00
License: CC-BY-4.0