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Extreme snowfalls and atmospheric circulation patterns in the cantabrian mountains (nw Spain)

dc.contributor.authorGarcía Hernández, Cristina 
dc.contributor.authorLópez Moreno, J. I.
dc.date.accessioned2024-07-11T07:31:39Z
dc.date.available2024-07-11T07:31:39Z
dc.date.issued2024
dc.identifier.citationCold Regions Science and Technology, 221 (2024); doi:10.1016/j.coldregions.2024.104170
dc.identifier.issn0165-232X
dc.identifier.urihttps://hdl.handle.net/10651/73445
dc.description.abstractDuring winter, ice cover frequently forms on the water surface of rivers with vegetated channel beds in cold regions. The investigation of the impacts of both ice cover and channel bed vegetation on flow structures around bridge abutments is essential for engineers to gain a comprehensive understanding of the complex interactions occurring in such a situation. In the present study, the flow structure around a rectangular bridge abutment in the presence of vegetation under ice-covered conditions has been studied. Considering different vegetation densities by arranging vegetation elements in square and staggered configurations, this study incorporates the influence of ice covers with different roughness, namely smooth and rough ice cover. Key turbulence parameters, including turbulence intensity, Reynolds shear stress (RSS), and turbulent kinetic energy (TKE), are also examined based on laboratory experiments. Results show that the shape of velocity profiles for flow over a vegetated channel bed changes from an S-shaped curve under an open flow condition to a convex shape under ice-covered conditions. The effects of an ice cover and vegetation on the flow around the bridge abutment create unpredictable turbulence intensity patterns. Under a rough-covered flow condition, there appears a larger area with negative Reynolds shear stress (RSS) downstream of the abutment. Turbulent kinetic energy (TKE) under ice-covered conditions has substantially lower magnitudes than in open flow conditions.
dc.description.sponsorshipThe Natural Sciences and Engineering Research Council of Canada (NSERC) under the Discovery Grant Program RGPIN-2019-04278.
dc.language.isoeng
dc.relation.ispartofCold Regions Science and Technology
dc.rightsCC Reconocimiento 4.0 Internacional  
dc.rights© 2024 The Authors. Published by Elsevier B.V.
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.sourceScopus
dc.source.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85187173566&doi=10.1016%2fj.coldregions.2024.104170&partnerID=40&md5=8917d7474611a74132ca1612320f4668
dc.titleExtreme snowfalls and atmospheric circulation patterns in the cantabrian mountains (nw Spain)
dc.typejournal article
dc.identifier.doi10.1016/j.coldregions.2024.104170
dc.local.notesOA ATUO24
dc.relation.projectIDRGPIN-2019-04278
dc.relation.publisherversionhttp://dx.doi.org/10.1016/j.coldregions.2024.104170
dc.rights.accessRightsopen access


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