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dc.contributor.advisorChairperson, Graduate Committee: Katherine J. Hansen; Karl W. Birkeland (co-chair)en
dc.contributor.authorCooperstein, Michael Stephenen
dc.date.accessioned2013-06-25T18:42:38Z
dc.date.available2013-06-25T18:42:38Z
dc.date.issued2008en
dc.identifier.urihttps://scholarworks.montana.edu/xmlui/handle/1/1107en
dc.description.abstractThis research was conducted to determine if slope aspect played a role in the formation, size and shape of surface hoar and near-surface faceted crystals and on the meteorological variables that are known to result in the formation of these two weak layers. No studies have specifically studied the effects of slope aspect on the size and shape of these crystals nor the effects of slope aspect on the meteorological variables which are known to result in differences in temperature and vapor pressure gradients and ultimately result in the formation of two weak layers.en
dc.language.isoenen
dc.publisherMontana State University - Bozeman, College of Letters & Scienceen
dc.subject.lcshAvalanches.en
dc.subject.lcshForecasting.en
dc.subject.lcshFrost.en
dc.subject.lcshSnow Thermal properties.en
dc.titleThe effects of slope aspect on the formation of surface hoar and diurnally recrystalized near-surface faceted crystalsen
dc.typeThesisen
dc.rights.holderCopyright 2008 by Michael Stephen Coopersteinen
thesis.catalog.ckey1410163en
thesis.degree.committeemembersMembers, Graduate Committee: Stephan G. Custeren
thesis.degree.departmentEarth Sciences.en
thesis.degree.genreThesisen
thesis.degree.nameMSen
thesis.format.extentfirstpage1en
thesis.format.extentlastpage169en


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