Show simple item record Iacozza, John en_US 2007-05-15T19:04:52Z 2007-05-15T19:04:52Z 1997-08-01T00:00:00Z en_US
dc.description.abstract In this thesis, the distribution of snow over first-year (FYI), multiyear (MYI) and rubble (RI) sea ice were measured at 15 sites sampled during two years of field research in the Canadian Arctic. A geostatistical technique known as the variogram was used to model the statistical pattern of the snow distribution. The variogram examines the spatial continuity of a regionalized variable and how this continuity changes as a function of distance and direction. Results indicate that the variogram provided a good estimate of the type and change of spatial dependence on the snow depths over the various ice types. Over FYI, the regular smooth ice topography produced a periodicity in the snow drifts that was best estimated using a wave theoretical variogram in combination with a gaussian model. The more irregular ice topography characteristic of MYI and RI produced a more irregular snow drift pattern. The most appropriate models were a combination of the spherical and gaussian variogram models. Geometric anisotropy was present in all 15 sites, indicating a directional trend in the spatial continuity of the snow distribution patterns which was attributed to the prevailing wind vector during depositional storm events. These distribution models were used to estimate the spatial dispersion of the photosynthetically active radiation (PAR) transmittance through the snow and ice covers on the arctic oceans. This application of the models illustrated the importance of snow distribution on the transmittance of PAR. Plots of the transmittance for each ice type were produced. (Abstract shortened by UMI.) en_US
dc.format.extent 13137037 bytes
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dc.language en en_US
dc.language.iso en_US
dc.title Models of snow distribution patterns for various types of sea ice in the Canadian high Arctic en_US Geography en_US Master of Arts (M.A.) en_US

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