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<br />()S2S <br /> <br />100 <br /> <br /> * <br />0 DAILY ANALYSIS (J @ <br />II STREAMFLOW. * ~ <br />EVENT ANALYSIS * <br /> * <br />* * * <br /> <br />Cl <br />Z <br />o 80 <br />() <br />w <br />'" <br />ffi 60 <br />a. <br />~ ~ <br />u. ..... 40 <br />() <br />10 <br />B 20 <br />;!; <br />~-O <br />g <br />a: <br />o .20 <br />Z <br /> <br />~ z .40 <br />;: :;: <br />g '" <br />u.. <br />::; .60 <br />Lli <br />a: <br />~ -80 <br /> <br /> <br />I <br /> <br />.100 <br /> <br />NOTE: NOT ALL OUTLIERS <br />ARE SHOWN <br /> <br />~ <br /> <br />.120 <br /> <br />o <br />SPRING <br /> <br />WINTER <br /> <br /> <br />. <br /> <br />SUMMER <br /> <br />FALL <br /> <br />SEASON <br /> <br />Figure 11. Boxplots showing daily mean streamflow gains and losses and daily mean streamflow-event <br />gains and losses for reach 3 of the study area, 1984-92. : <br /> <br />CONFIDENCE IN ACCURACY <br />OF ESTIMATES <br /> <br />Overall confidence in the estimation of stream- <br />flow traveltimes and of streamflow gains and losses <br />using historical streamflow and diversion records was <br />considered to be good to fair for reaches 2 and 3, <br />which compose about 100 mi of the lower Purgatoire <br />River. Because available information was insufficient <br />to quantify the return flows and other tributary contri- <br />butions (ungaged inflows) in reach 3, the magnitude of <br />errors in assuming that ungaged streamflow in an <br />irrigated river reach generally was inconsequential <br />could not be evaluated directly. The streamflow-event <br />analyses that were made for reaches 2 and 3 did help <br />to strengthen the confidence ih the accuracy of the <br />reported estimates of streamflow gains and losses for <br />these two reaches. <br />The hydrologic data available for reach I did <br />not provide adequate information to estimate stream- <br />flow traveltime and to determine streamflow gains and <br /> <br />josses accurately. Additional information that could <br />Improve confidence in traveltime estimates and <br />quantify streamflow gains and losses for specific flow <br />conditions better include: <br /> <br />,1. Dye-tracer studies conducted dnring two or more <br />. flows, preferably a low flow and a high flow, to <br />determine traveltimes for the transport of stream- <br />I flows to downstream river locations. <br />I <br />~. Identification and quantification of ungaged inflows <br />! to the lower Purgatoire River system, including <br />the extent of operational practices by canals <br />(sluicing); the surface routing of irrigation field <br />tailwater, waste flows, and other sources of return <br />flows; and the magnitude of streamflow contribu- <br />tions by tributary streams. <br />I <br />i Determination of streamflow traveltime and <br />petter estimates of streamflow gains and losses <br />in a complex irrigated surface-water and ground- <br />'water system, such as in the lower Purgatoire <br />River, conld be approximated by the nse of computer <br /> <br />22 Evaluation of Streamflow Traveltime and Streamflow Gains and Losses along the Lower Purgatoire River, . <br />Southeastern Colorado, 1984-92 I <br />! <br />I <br /> <br />