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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />4 <br /> <br />fact, both states anticipated and intended that the <br /> <br /> <br />usable stateline flows would increase after the Compact <br /> <br /> <br />became effective, <br /> <br />2, Arkansas River at Las Animas - In addition to the normal <br /> <br /> <br />flows of the Arkansas River at Las Animas, deliveries of <br /> <br /> <br />water are made to John Martin Reservoir to be stored in <br /> <br /> <br />accounts owned by users located upstream of the reser- <br /> <br />voir, Such deliveries do not constitute native flow of <br />the Arkansas River but are included in the measured flow <br />at the gage near Las Animas, Such flows must be sub- <br />tracted from the gaged flows to determine the natural <br />flow at the gage, This adjusted flow is the amount of <br />water stored in John Martin Reservoir and eventually re- <br />leased to downstream users in Colorado and Kansas pur- <br />suant to the Compact. The practice of delivering other <br />water into John Martin Reservoir started in 1977, Most <br />of this other delivered water has resulted from the <br />operation of the Winter Water Storage Program on the <br />Arkansas River, in which water is stored in lieu of <br />direct flow diversions for irrigation 4uring the winter, <br />As part of this program, water is stored in John Martin <br />Reservoir for several participants, Storage of program <br />water occurs during the months of November through March, <br />Records of winter water flows at the Las Animas gage are <br />