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<br />11 <br />CLIMATE <br />The climate of the Virgin River basin ranges from aril in the <br />valley floors in the southern part of the basin to humid in the <br />mountains to the north. Over most of the basin the climate is grid <br />to semiarid, with little precipitation, mild winters, hot summers <br />and high evaporation rates. <br />The climatic pattern of the Virgin River basin is typical of <br />the Southwest: a biseasonal regime characterized by two periods of <br />precipitation (winter and summer) and Cara periods of drought (spring <br />and fall)(Lowe-1964 and references cited therein). The greatest <br />amount of precipitation occurs from December through March (regional <br />storms) as snow in the mountains and rain at the lower elevations. <br />In the summer precipitation is commonly localized thunderstorms which <br />result in rapid runoff (fl-ash fi~ooding is common) and much erosion <br />(Cordova et al. 1972, Glancy and Van Denburgh 1959;. In general <br />the northwesterly grinds of winter and the southwesterly winds of <br />summer control precipitation while differences in altitude determine <br />the temperature ". but the influence of these factors is so <br />~greatiy modified by topography that each deep canyon, wide valley, <br />broad slope, and plateau top seems to have a climate of its own" <br />(Gregory 1950, p. 28). - <br />~ .. .. <br />Mean monthly and annual temperatures for selected stations are <br />presented in Table ]. Mean monthly and annual precipitation records <br />for selected stations are presented in. Table 2. The average annual <br />precipitation over the entire basin is approximately 30 cm and <br />