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<br />D R AFT <br /> <br />SECTION V - WINTER OROGRAPHIC PRECIPITATION <br />MANAGEMENT - PRESENT LEVEL OF UNDERSTANDING <br /> <br />s <br /> <br />The potential to increase the amount of water available in the <br />western United States and specifically within the Colorado River <br />Basin lies primarily in the ability to increase winter snowfall. <br />Additional water pr'oduced by seeding winter orographic clouds is <br />released for irrigation, domestic, and energy use when the snow melts <br />and runs off in thE~ late spring and summer. <br /> <br />A. Basic Principles <br /> <br />Clouds are produced when three basic conditions are present in the <br />atmosphere: (1) there is a sufficient quantity of moisture in the <br />form of water vapor', (2) there is a mechanism by which air is cooled <br />to the water saturation point and beyond, and (3) there is a sufficient <br />quantity of small aerosol particles to act as condensation nuclei. <br />Clouds form when air rises, expands, and cools causing water vapor to <br />condense producing liquid water in the form of cloud droplets. <br /> <br />~ <br /> <br />Precipitation in the form of snow is produced when ice crystals form <br />around ice nuclei. These ice crystals then grow at the expense of <br />the supercooled (bE!low freezing) cloud droplets until they are large <br />enough to fall as snow. To increase the precipitation from a cloud, <br />its ability to convert cloud liquid water to precipitation must be <br /> <br />39 <br />