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<br />I <br />1 <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />, <br />I <br />I <br />I <br />J <br />I <br /> <br />1 <br /> <br />1. INTRODUCTION AND BACKGROUND <br /> <br />1.1 Introduction <br />In many mountainous regions around the world, hydrologists and <br />meteorologists have pointed out the effects of topography on winter <br />precipitation and have tried to find a scientifically sound explanation <br />for the phenomenon. Because an accurate diagnostic and predictive <br />knowledge of the temporal and spatial distribution of winter precipita- <br />tion in mountainous regions is of considerable importance to a wide <br />range of populations, the idea of using a computer model to address this <br />problem arose about three decades ago, and some attempts were conclusive <br />to a certain degree. <br />Morocco was subject to below normal rainfall conditions during most <br />of the 1970's and early 1980's. The period extending from 1979 to 1983 <br />has been exceptionally dry. Due to the length of the drought, most of <br />the reservoirs across the country were reduced to an average of 10% of <br />their designed water storage capacity. The social and economic impact <br />of this serious situation, considered to be the worst in modern history, <br />were aggravated by the increased demand for additional water resources <br />caused by population growth, industrialization, urbanization, and expan- <br />sion of irrigation. <br />As a consequence of this situation, the government of Morocco <br />fllrmulated an official request for technical assistance in weather <br />modification to the government of the United states of America, after <br />which, a team of American experts recommended a weather modification <br />pl'ogram with emphasis on winter snowpack augmentation in the High Atlas <br />Mountains. <br />