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<br />Representative streamflow for three hydrologic regimes <br />(data are from 1967) <br /> <br />50 <br /> <br />-snov.melt (Elk River at Clark) <br />-monsoonal (Purgatoire River near Thatcher) <br />-ground water (Arikaree River at Haigler) <br /> <br />Elk River <br /> <br />>: 45 <br />o <br />E <br />'" 40 <br />Q) <br />>: 1;; 35 <br />.2>> <br />Em <br />'" -0 30 <br />~ c <br />~ ~ 25 <br />Q)- <br />~ >: <br />~ .g 20 <br />o ~ 15 <br />z ~ <br />; 10 <br />'iij <br />9- 5 <br /> <br />. Of :.; <br /> <br />.,~ <br /> <br />, <br /> <br /> <br />0 <br />r- r- r- r- r- r- r- r- r- r- r- r- <br /><0 <0 <0 <0 <0 <0 <0 <0 <0 <0 <0 <0 <br />(J) (J) (J) (J) (J) (J) (J) (J) (J) (J) (J) (J) <br />~ N ?i ~ LO iO j:::: co OJ 25 ~ N <br /> ~ <br /> <br />Hydrologic patterns vary among stream types, so the type of <br />non-consumptive attribute supported may also vary <br /> <br />Flow Relationships to Non-consumptive <br />Attributes <br /> <br />· High flows, including small and large floods <br />- Naturally occur during runoff <br />- Examples of functions they provide: <br />. Structuring habitat <br />. Removing sediment <br />. Cottonwood seedling establishment <br />- Characterized by magnitude, timing, duration, <br />frequency, and rate of change <br />- Methods for determining characteristics are <br />mostly hydrology-based <br /> <br />30 <br /> <br />15 <br />