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dc.contributor.authorLang, Renee M.en
dc.date.accessioned2015-05-09T18:56:35Z
dc.date.available2015-05-09T18:56:35Z
dc.date.issued1985en
dc.identifier.urihttps://scholarworks.montana.edu/xmlui/handle/1/3999en
dc.description.abstractField studies on surface hoar were conducted during the winter months of 1982-83 and 1983-84, at the Big Sky Ski Area, Big Sky, Montana. Mechanical shear strength tests, conducted on established surface hoar layers, indicated that although a layer would become visually undetectable, shear strength remained too low to measure for extended periods of time. The initiation of surface hoar growth was dependent on a variety of near-surface and atmospheric conditions. Nocturnal clear-sky radiative heat loss from the snow surface did not necessarily predispose condensation onto the surface, although near-surface air temperature gradients would be in excess of +200°C/m. A steady-state approximation for conservation of mass and momentum, in conjunction with the temperature data, predicts that surface crystal growth cannot be a diffusion limited process.en
dc.language.isoenen
dc.publisherMontana State University - Bozeman, College of Engineeringen
dc.subject.lcshFrosten
dc.subject.lcshAvalanchesen
dc.titleStudies on surface hoar : formation and physical propertiesen
dc.typeThesisen
dc.rights.holderCopyright Renee Maria Lang. 1985en
thesis.catalog.ckey339560en
thesis.degree.departmentCivil Engineering & Engineering Mechanics.en
thesis.degree.genreThesisen
thesis.degree.nameMSen
thesis.format.extentfirstpage1en
thesis.format.extentlastpage56en


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