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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br /> <br />Storm Dynamics <br /> <br />Large-scale Flow Patterns <br /> <br />Figure S. Schematic diagram showing relative importance of factors that result in precipitation <br /> <br />The large-scale hemispheric flow is the major factor that produced the deserts of the world located <br />about 30 degrees north and south latitudes. It also interacts with other factors to produce the mild <br />and wet climates around the earth. The large-scale flow associated with jet stream winds is the <br />predominant factor that interacts with other atmospheric features and influences winter precipitation <br />patterns in Utah. These patterns are large-scale guides to precipitation producing storms. <br /> <br />11 <br /> <br /> <br />Figures 6 and 7 show schematics of general large-scale hemispheric flow over the Western United <br />States. Figure 6 represents the type of large-scale flow that persisted during the wet, 1971-1975 and <br />1979-1988 winters. Figure 7 represents the large-scale flow patterns that persisted during the dry <br />winters of 1976-1977 and 1989-1990. <br /> <br />Droughts and wet spells in the State of Utah are inter-related with events on a global scale. The <br />position and movement of the Intertropical Convergence Zone (lTCZ), EI Nino, ocean water surface <br />