Thesis (Ph. D.)--Carleton University, 1989. / Also available in electronic format on the Internet.

Thesis (Ph.D.)--York University, 2007. Graduate Programme in History. / Typescript. Includes bibliographical references (leaves 252-278). Also available on the Internet. MODE OF ACCESS via web browser by entering the following URL: http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&res_dat=xri:pqdiss&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft_dat=xri:pqdiss:NR32069

No description available.

Thesis (Ph.D.)--McMaster University, 2003. / Advisor: Richard Harris. Includes bibliographical references (leaves 300-320). Also available via World Wide Web.

Thesis (Ph.D.). / Written for the Dept. of Geography. Maps in pocket. Bibliography: leaves [377]-385.

Thesis--University of Michigan. / Caption title. Extracted from Transactions of the Royal Canadian Institute, Oct. 1949, v. 28, pt. 1. Bibliography: p. 117-118.

The crustal thickness and P velocities in the Port Arthur, Ontario region of the Canadian Shield have been previously determined by seismic refraction techniques during the Lake Superior Experiment and Project Early Rise. In this study, the P phases of eleven teleseismic earthquakes recorded near Port Arthur have been studied by computing azimuths, angles of incidence, and spectral ratios to ascertain some crustal properties and compare these values with the refraction results. A P velocity at the surface of 6.1 ± .8 km/sec and a crustal thickness of 40 ± 5 km determined from the earthquakes are similar to but less precise than the refraction estimates of 6.3 km/sec and 38 km respectively. Transverse motions generated by the earthquake signal passing through the crust were observed and contributed to the uncertainty. / Science, Faculty of / Earth, Ocean and Atmospheric Sciences, Department of / Graduate

No description available.

The lake breeze is shown to develop on 30% of all summer days in the Toronto region, similar to other findings in the Great Lakes area. Simulations with the Colorado State University (CSU) model show that under northwest to north gradient flow the lake breeze is characterized by a broad band of westerlies over the lake, while southwesterly gradient flow produces a broad band of easterlies. A nocturnal mesoscale cyclonic eddy is predicted over western Lake Ontario under west and northwest gradient flow conditions. / A statistical model intercomparison of the CSU and Ontario Ministry of Environment models over a 19600 km$ sp2$ domain centred on Pickering, ON revealed the CSU model generally more accurately predicts the temporal and spatial lake breeze characteristics. This is attributed to improved model parameterizations and larger domain size enabling the model to resolve the full-lake scale circulations which develop.

Thesis (Ph.D.) -- McMaster University, 1999. / Includes bibliographical references (leaves 203-224). Also available via World Wide Web.