Dalrymple, Paul Clement2018-07-312018-07-3119631963b14687203https://hdl.handle.net/2144/30099Thesis (Ph.D.)--Boston UniversityThe Antarctic Plateau is defined on the basis of elevation and slope, being above 2000 meters and with less than a one-degree slope in East Antarctica and being above 1500 meters with less than a one-degree slope in West Antarctica. This region is presented as a high latitude, high elevation, cold desert. It is shown to be a near homogenous geographical region, with a uniform snow surfaace, relatively little local relief, and great depths of snow. Its climate is controlled to a large degree by its geographical location. Elevation, slope, and distance from the coast are presented as the three most important geographical elements [TRUNCATED]en-USBased on investigation of the BU Libraries' staff, this work is free of known copyright restrictions.ClimatologyAntarcticaClimateThesis/Dissertation1171902566400699175769400001161