Modelling Hazardous Surface Hoar Layers in the Mountain Snowpack over Space and Time

atmire.migration.oldid3820
dc.contributor.advisorJamieson, Bruce
dc.contributor.authorHorton, Simon
dc.date.accessioned2015-11-03T20:16:14Z
dc.date.embargolift2016-02-22T07:00:00Z
dc.date.issued2015-11-03
dc.date.submitted2015en
dc.description.abstractSurface hoar layers are a common failure layer in hazardous snow slab avalanches. Surface hoar crystals (frost) initially form on the surface of the snow, and once buried can remain a persistent weak layer for weeks or months. Avalanche forecasters have difficulty tracking the spatial distribution and mechanical properties of these layers in mountainous terrain. This thesis presents numerical models and remote sensing methods to track the distribution and properties of surface hoar layers over space and time. The formation of surface hoar was modelled with meteorological data by calculating the downward flux of water vapour from the atmospheric boundary layer. The timing of surface hoar formation and the modelled crystal size was verified at snow study sites throughout western Canada. The major surface hoar layers over several winters were predicted with fair success. Surface hoar formation was modelled over various spatial scales using meteorological data from weather forecast models. The largest surface hoar crystals formed in regions and elevation bands with clear skies, warm and humid air, cold snow surfaces, and light winds. Field surveys measured similar regional-scale patterns in surface hoar distribution. Surface hoar formation patterns on different slope aspects were observed, but were not modelled reliably. Mechanical field tests on buried surface hoar layers found layers increased in shear strength over time, but had persistent high propensity for fracture propagation. Layers with large crystals and layers overlying hard melt-freeze crusts showed greater signs of instability. Buried surface hoar layers were simulated with the snow cover model SNOWPACK and verified with avalanche observations, finding most hazardous surface hoar layers were identified with a structural stability index. Finally, the optical properties of surface hoar crystals were measured in the field with spectral instruments. Large plate-shaped crystals were less reflective at shortwave infrared wavelengths than other common surface snow grains. The methods presented in this thesis were developed into operational products that model hazardous surface hoar layers in western Canada. Further research and refinements could improve avalanche forecasts in regions prone to hazardous surface hoar layers.en_US
dc.identifier.citationHorton, S. (2015). Modelling Hazardous Surface Hoar Layers in the Mountain Snowpack over Space and Time (Doctoral thesis, University of Calgary, Calgary, Canada). Retrieved from https://prism.ucalgary.ca. doi:10.11575/PRISM/26956en_US
dc.identifier.doihttp://dx.doi.org/10.11575/PRISM/26956
dc.identifier.urihttp://hdl.handle.net/11023/2626
dc.language.isoeng
dc.publisher.facultyGraduate Studies
dc.publisher.institutionUniversity of Calgaryen
dc.publisher.placeCalgaryen
dc.rightsUniversity of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.
dc.subjectPhysical Geography
dc.subjectRemote Sensing
dc.subjectEngineering--Civil
dc.subject.classificationSurface hoaren_US
dc.subject.classificationavalancheen_US
dc.subject.classificationMountain weatheren_US
dc.subject.classificationPersistent weak layeren_US
dc.subject.classificationNumerical weather predictionen_US
dc.titleModelling Hazardous Surface Hoar Layers in the Mountain Snowpack over Space and Time
dc.typedoctoral thesis
thesis.degree.disciplineCivil Engineering
thesis.degree.grantorUniversity of Calgary
thesis.degree.nameDoctor of Philosophy (PhD)
ucalgary.item.requestcopytrue
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