Correlating Surface Shear Stress to Realistic Complex Terrain in Stable Atmospheric Boundary Layers

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Correlating Surface Shear Stress to Realistic Complex Terrain in Stable Atmospheric Boundary Layers | 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 Correlating Surface Shear Stress to Realistic Complex Terrain in Stable Atmospheric Boundary Layers Majed Wardeh, Peter J. Disimile This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-7811586/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 This paper presents computational surface shear stress results of Atmospheric Boundary Layer flow over a domain of complex terrain representative of Cincinnati, Ohio. The computational data, generated using a time averaged turbulence closure model, is used to assess flow separation and reattachment patterns, as well as the influence of canopies modelled as surface roughness on the flow behavior. The present data is combined with a different dataset generated by Large Eddy Simulation and is used to produce a correlation that relates the surface shear stress over a single hill within real repeated hills to the hill’s geometry. The correlation displays a linear pattern between the growth of a hill’s downstream slope and the shear stress difference over the slope. The correlation can also act as a validation tool for future data measured or computed over complex terrain, and as a relation that explains flow separation and reattachment patterns over complex terrain. Atmospheric Boundary Layer Complex Topography Computational Fluid Dynamics Surface Shear Stress Turbulence Modelling Full Text Additional Declarations No competing interests reported. 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. 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