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Streamflow measurments define gage height- discharge <br />relation. <br />USGS technicians measure discharge or flow at all gaging <br />stations on a routine schedule. Measurements of water depth and <br />velocity are made at approximately 30 locations across the stream. <br />The distance between measurement locations (width), the speed of <br />the water (velocity), and water depth are multiplied to compute <br />discharge (or streamflow) in cubic feet per second (ft3 /s). Many of <br />these measurements made over the range in stage of the stream are <br />plotted against the corresponding stages to define the stage - <br />discharge relation that is used in conjunction with the recorded <br />stage to determine continuous discharge throughout the year. <br />Canoeist enjoying the Kansas <br />River at Burcham Park in <br />Lawrence, Kansas. <br />1,000,00 <br />a <br />0 <br />N 100,000 <br />a) <br />CL <br />N <br />a 10,000 <br />U <br />C <br />3 <br />0 <br />E 1,000 <br />CO <br />P <br />n <br />USGS technician measuring discharge on the Kansas <br />River at Lecompton. <br />IRISH 111111.....11.11.. ��M7C7:7::1111 °�OIIILIC ::::...... :::t 111•11110....... 111....11: "1 n11 mmm�o.n ll•nn.NInn11111111n1111 <br />NIINI.N.NIIIIIIn1111111NIIININ, INIINBNNNIN.::1111011.. EEWHO,14 11 NINIn11n.NNIIIn11NNI 11 IIIIIIIININ..1.11 III........ <br />00...1::.M 111 .:V.. 7 " :....M.Cn. <br />.p::::ll::::: 1 Iln....fi!I��.ff�' /7: INn1:111111.A1:....1 WWMR :::..1.1 1111111:::: 11::: 1:::::: Nolen ::::::::::111'111111:::IIIall <br />2 <br />1A <br />1 <br />.. a 6 9 Pa 9 9 g g s <br />DISCHARGE, IN CUBIC FEET PER SECOND - " <br />Stage- discharge relation for Kansas River at Lecompton. <br />06891000 Kansas River at Lecompton (site 8) <br />Long -term median daily streamflow Streamflow via satellite 1 <br />(based on 60 years of record) <br />100' 1 1 1 I I I 1 <br />22 23 24 25 26 27 28 29 <br />May 1997 <br />Hydrograph of flow for Kansas River at Lecompton from INTERNET. <br />Discharge graphs <br />Continuous discharge information at <br />gaging stations, like this "hydrograph" <br />of the flow of the Kansas River at <br />Lecompton, is useful to boaters and <br />other recreational users. Because <br />discharge is related to stream velocity, <br />those experienced with the river can <br />relate discharge information to how fast <br />the water is moving down the stream. <br />For example, veteran boatmen on the <br />Kansas River have been able, through <br />experience, to determine a relationship <br />between the river's discharge and good <br />or poor boating conditions. <br />