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<br />ABSTRACT OF THESIS <br />WINTERTIME CLOUD SYSTEMS OVER THE COLORADO ROCKIES: THREE CASE STUDIES <br /> <br />~ <br /> <br />'I> <br /> <br />This study focuses upon the mechanisms by which mountains and <br /> <br />synoptic weather systems interact to produce characteristic orographic <br /> <br />cloud systems. In each of the three case studies, a synoptic cloud <br /> <br />component, an orographic cloud component~, and a convective cloud compo- <br /> <br />nent were identified through the analysis of rawinsonde data, vertically <br /> <br />pointing radar data, and visual observations. <br /> <br /> <br />The follo"ring are considered to be the major findings of this <br /> <br /> <br />study: i) wintertime cloud systems over the Colorado Rockies form by <br /> <br /> <br />vertical velocity components which act on different size and time scales <br /> <br />(synoptic, orographic, and convective); i.i) at times, a fourth cloud <br /> <br />component, generated by the mesoscale structure of the synoptic distur- <br /> <br />bance (e.g., travelling gravity wave, moving convective bands, or organ- <br /> <br />ized convective lines, etc.) invigorates the entire cloud system, <br /> <br />iii) upwind blocking is very important to the orographic lift and the <br /> <br />lifted cloud system; iv) the deduced cloud is very sensitive to the <br /> <br /> <br />lifting model and the upwind profiles of temperature and moisture; and <br /> <br />v) synoptic storm tracks, travelling mesoscale phenomena, large scale <br /> <br />vorticity, moisture and temperature advection, synoptic and topographic <br /> <br />forcing of wind direction and speed, vertical structure of temperature <br /> <br />and moisture, cold air pooling, nocturnal valley inversions, blocking, <br /> <br />and stagnation all constitute controls on orographic cloud systems. <br /> <br />The timing and interaction of the above physical processes deter- <br /> <br />mine the formation and behavior of the cOTIlplete cloud system and define <br /> <br />'" <br /> <br />... <br /> <br />iii <br />