Change characteristics of the Induced Geoelectric Field Observed by China Geoelectric Network During the Extreme Magnetic Storm of May 11, 2024

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Abstract In this paper, we analyze the characteristics of the induced geoelectric field in mainland China during the extreme magnetic storm from May 10–12 2024, based on the data from China Geoelectric Network. Our analysis focuses on the magnitude of the induced geoelectric field changes, the ratio between isotropic short and long dipoles, and the variation in polarization direction across different regions during the sudden onset of the magnetic storm. Our study reveals that horizontal changes in the induced geoelectric field intensity are not confined to specific regions during the sudden onset magnetic storms. When analyzing the same-direction ratio, at most stations it showed a consistent ratio between short and long dipoles. The polarization orientation derived from long-dipole ratios suggests that there is no consistent alignment of land and sea directions on the ground surface. These results indicate that the variations in geoelectric field measurements are influenced by the underlying electrical structure at each station. These findings are further interpreted by using high-density electric exploration data. This paper provides a quantitative characterization of changes in the induced geoelectric field intensity across mainland China during the geomagnetic storms, offering a foundation for further analysis of regional geoelectric field electromagnetic phenomena.
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Change characteristics of the Induced Geoelectric Field Observed by China Geoelectric Network During the Extreme Magnetic Storm of May 11, 2024 | 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 Change characteristics of the Induced Geoelectric Field Observed by China Geoelectric Network During the Extreme Magnetic Storm of May 11, 2024 Wenzhou Zhao, Qinzhong Ma, Wei Li, Lanwei Wang, Yu Zhang, Yanlin Wen This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-5472086/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 In this paper, we analyze the characteristics of the induced geoelectric field in mainland China during the extreme magnetic storm from May 10–12 2024, based on the data from China Geoelectric Network. Our analysis focuses on the magnitude of the induced geoelectric field changes, the ratio between isotropic short and long dipoles, and the variation in polarization direction across different regions during the sudden onset of the magnetic storm. Our study reveals that horizontal changes in the induced geoelectric field intensity are not confined to specific regions during the sudden onset magnetic storms. When analyzing the same-direction ratio, at most stations it showed a consistent ratio between short and long dipoles. The polarization orientation derived from long-dipole ratios suggests that there is no consistent alignment of land and sea directions on the ground surface. These results indicate that the variations in geoelectric field measurements are influenced by the underlying electrical structure at each station. These findings are further interpreted by using high-density electric exploration data. This paper provides a quantitative characterization of changes in the induced geoelectric field intensity across mainland China during the geomagnetic storms, offering a foundation for further analysis of regional geoelectric field electromagnetic phenomena. Geoelectric field Geomagnetic storm Induced electric field intensity Full Text Supplementary Files GraphicalAbstract.png 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. 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-5472086","acceptedTermsAndConditions":true,"allowDirectSubmit":true,"archivedVersions":[],"articleType":"Research Article","associatedPublications":[],"authors":[{"id":387862203,"identity":"8ac66fd2-1695-429b-acf0-10a0685df172","order_by":0,"name":"Wenzhou 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