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hydrograph that mimics natural flows and <br />provides a diversity of opportunities. The prob- <br />lem is that information relating flows to <br />resource values typically does not identify the <br />percent of water that can be removed without <br />impacting those values, but rather the static <br />flow needed to provide them. <br />One way to circumvent this problem is to <br />develop percentage -based requests after ini- <br />tially determining the total amount of water <br />needed for a trigger request (there are other <br />methods that could be used to develop a <br />defensible percentage; exploring these is <br />beyond the scope of the present paper). Using <br />this method, the percentage -based request <br />asks for the same total amount of water as the <br />trigger request, but in an alternative way that <br />is easier to administer and which provides <br />greater diversity through the flow range. <br />Trigger requests are different in years with <br />different natural flows, so percentages based <br />on trigger requests for different years (i.e., wet <br />versus dry years) will vary. The natural flow <br />regime used to develop the percentage could <br />be based on an agreed -upon "typical" year, or <br />an average of several years. For simplicity and <br />the illustrative purposes of this paper, calcula- <br />tions here were made for a single year (1995). <br />Based on mean annual flows from the period <br />of record, this was a wetter than average year. <br />The trigger request for 1995 (Figure 3) <br />asked for 73.5% of the water available in that <br />year. Applying this percentage, we devel- <br />oped the percentage -based request shown in <br />Figure 4. On any given day, the flow request is <br />for 73.5% of the available water. The resulting <br />hydrograph mimics the natural hydrograph, <br />but at a lower level. <br />Advantages <br />• Instream values are identified with flow <br />ranges rather than specific thresholds. For <br />many resources, a continuum of flows bet- <br />ter protects resources than a single flow. <br />• Allows protection of needed flows whenev- <br />er they occur. <br />• Requests higher flows during rare high <br />flow events, protecting associated recre- <br />ational opportunities such as challenge -ori- <br />ented whitewater boating. <br />• Recognizes that natural flow regimes may <br />differ each year. Allows for lower requests <br />in dry years and higher requests in wetter <br />years, which is likely to better maintain bio- <br />physical conditions (Hill et al. 1991). <br />• Provides a more incremental regime, which <br />mimics natural flows. <br />• May allow easier administration of out -of- <br />stream flows in some situations. Although <br />percentage -based requests are probably <br />more challenging to administer when flows <br />are provided from an upstream dam (thus <br />requiring daily adjustments), they may be <br />easier to administer when there are a series <br />of junior diversions involved. Junior users <br />always have to adjust their diversions in <br />times of shortage, and a percentage -based <br />system actually simplifies the number of <br />times that happens in comparison to trigger <br />requests. For example, on rivers with "flashy" <br />spring or winter high flow periods and a <br />more predictable falling limb of the hydro - <br />graph during the ' summer, it is the latter <br />period when out -of- stream demand usually <br />exceeds supply. In these cases, a percent- <br />age -based request requires each junior user <br />to sequentially stop diverting (when the dif- <br />ference between natural flows and the per- <br />centage- derived amount is equal to the sum <br />of senior water rights). With a trigger system, <br />they may have to cease and then begin <br />diverting as flows pass through each <br />threshold. <br />• Allows for less precision in choosing thresh- <br />olds for resource needs because a range of <br />flows is provided. This fits with the consis- <br />tent finding in recreation research that flow <br />evaluations are incremental and have some <br />variation (Shelby et al. 1992b; Whittaker et <br />al. 1993). <br />Disadvantages <br />• The hydrograph resulting from the request <br />changes each year, depending upon water <br />availability. Junior out -of- stream users will <br />not know ahead of time how much water is <br />available. As previously noted, however, <br />junior water users are not assured of water <br />whenever a river is fully appropriated. <br />• Does not identify times when various flows <br />will be available; recreation users have to <br />plan their trips based on weather and run- <br />off predictions, which determine the actual <br />flows that will be provided. In this way, <br />percentage requests also require the kind of <br />planning needed for unregulated rivers. <br />• There may be negative effects associated <br />with percentage decreases that would not <br />occur with trigger requests. For example, if <br />1,000 cfs is the precise flow required to pro- <br />240 Rivers • Volume 7, Number 3 2000 <br />_ i <br />