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<br />I <br /> <br />;)~~2S1 <br /> <br />I <br /> <br />I <br /> <br />storage season activity is geared toward conserving and extending <br /> <br /> <br />available water supplies. As much water as possible is <br /> <br /> <br />introduced to storage. Efficient system regulation involves <br /> <br /> <br />d~ing up rivers at points of reservoir diversion. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />System operation during the irrigation season makes use of <br /> <br /> <br />natural flow, reservoir storage, and river accretions. During <br /> <br /> <br />th$ early portion of the season, water needs are satisfied by <br /> <br /> <br />direct runoff and return flows. High country snowmelt generally <br /> <br /> <br />occurs from mid-May to mid-June. In July and August, storage <br /> <br /> <br />releases are significant. Many ditches are supplied exclusively <br /> <br /> <br />by seepage and returns tributary to the main-stem river system. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Irtigation flows are often managed by sophisticated programs of <br /> <br /> <br />diversion and exchange. Water requirements of downstream senior <br /> <br /> <br />diverters may be satisfied by reservoir storage releases. Upstream <br /> <br /> <br />ditches may use exchanged river water. Flow in specific portions <br /> <br /> <br />of:the river may be exhausted in intervening reaches. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Delivery of water to various ditches may be accomplished through <br /> <br /> <br />canals, reservoirs, and ditches that bypass the main-stem channel <br /> <br /> <br />of .major rivers in the region. In instances where the river <br /> <br /> <br />channel is used to convey water to downstream users, these <br /> <br /> <br />supplies often sustain flows in stream reaches at high levels <br /> <br /> <br />that normally would not exist under unregulated conditions. A <br /> <br /> <br />call for stored water by a downstream ditch may determine to a <br /> <br /> <br />lange degree the volume of river flow passing upstream locations. <br /> <br />Fluptuating ditch headgate requirements cause concommitant <br /> <br />fluctuations in streamflow. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />2-5 <br /> <br />I <br /> <br />j <br /> <br />",:.i,_" <br /> <br />,jij.- <br /> <br />."j-j <br />~, <br />, <br />'I <br /> <br />~< ,,-; <br /> <br /> <br /> <br />