Changes in the physical properties of the atmosphere are caused by geographic influences and dynamic effects. The nature of the surface of the earth over which the air passes is usually the main factor in modifying the air in the lower levels of the troposphere. The ocean area of Hudson Bay in northeastern Canada presents an extensive surface for modification of air. Continental polar air crossing Hudson Bay and continuing into eastern Canada is modified not only by the underlying surface but also by the dynamic effects occurring in the atmosphere during its trajectory over these regions. The amount of modification is of major importance in the climate of the surrounding area, and in the meteorology of North American air masses. It was the purpose of this study: 1. To compute the changes in the physical properties that occur in continental polar air over Hudson Bay, Consequently, a project was undertaken to determine the amount of ice that forms on Hudson Bay in winter. The effect of the formation of ice in changing the modification of air was then studied. [...]

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This thesis is focused on determining the rate at which the climate of western North America (WNA) has changed in recent history, and looks at the impact that projected future climatic changes will have on a large glaciated watershed in the Canadian Rocky Mountains. The rate of change over WNA is quantified for 485 climate stations for the period 1950-2005 using indicators developed by the World Meteorological Organization (WMO). Results of the analysis show statistically significant historical trends across the study area. To gauge the effect of climate change on glaciers, a mass balance model was developed and integrated with the University of Lethbridge GENESYS hydrometeorological model. GCM future climate scenarios were used to model change in the Upper North Saskatchewan River Basin through 2100. Results forecast dramatic declines (> 80%) in total glacier area, ice volume, and streamflow contribution by 2100. / ix, 137 leaves ; 29 cm