Analyses of the atmosphere and its dynamics using surface radon fluxes and MST radar | 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 Analyses of the atmosphere and its dynamics using surface radon fluxes and MST radar Nagaraja Kamsali, Chakravarty S Subash This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-3808378/v1 This work is licensed under a CC BY 4.0 License Status: Under Review Version 1 posted 5 You are reading this latest preprint version Abstract An experiment was performed at Gadanki, India (13.5 N, 79.2 E) from October 17th to 22nd, 2011. The experiment involved measuring the concentration of atmospheric radon, as well as meteorological factors and MST radar signal strengths in tropo-stratosphere mode. The objective of this experiment was to examine the influence of convective activity on the vertical profiles of several parameters. A comparison has been conducted between the fluctuations of these parameters during the convective event that occurred on October 22, 2011, and data that is similar to that obtained on previous days. The results indicate a significant correlation between the upward movement of radon, the subsequent impact on the dispersion of water vapour, and the vertical structure of radar reflectivity and vertical winds. There has been a notable increase in the range of vertical wind at the period when convective activity was at its most advanced, and these observations are the first of this kind. Full Text Cite Share Download PDF Status: Under Review Version 1 posted Editorial decision: Reject, do not transfer 17 May, 2024 Reviewers agreed at journal 10 Apr, 2024 Reviewers invited by journal 07 Apr, 2024 Editor assigned by journal 31 Mar, 2024 First submitted to journal 31 Mar, 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. 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