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Instream Flows for Recreation: A Handbook on Concepts and Research Methods
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Instream Flows for Recreation: A Handbook on Concepts and Research Methods
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5/26/2017 12:41:36 PM
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Water Supply Protection
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Instream Flows for Recreation: A Handbook on Concepts and Research Methods
Date
1/1/1993
Author
Whittaker, Doug; Shelby, Bo; Jackson, William; Beschta, Robert - National Park Service
Title
Instream Flows for Recreation: A Handbook on Concepts and Research Methods
Water Supply Pro - Doc Type
Report/Study
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How River Environments Respond to Changes in Flow <br />Indirect effects of flow play important roles in creating and sustaining high quality recreation experiences <br />although it is often difficult to predict how changes in flows will change the river environment. Two examples of <br />how changes in flow regimes may affect important features are given below. <br />1. Sustained Decreases In Flow <br />A sustained decrease in flow throughout a year or season is a common situation with rivers across the country <br />as water is diverted for municipal water supply, industry, or agriculture. But what are the likely or possible effects of <br />decreased flows? Table 3 provides a list of possible effects for Beaver Creek, an alluvial river in Alaska, where <br />researchers explored these effects. If there were to be a sustained decrease in flows on that river, a number of <br />important physical features would change and thus affect the recreational opportunities on the river. A few of the <br />more important changes include decreases in size of gravel bars or beaches (detracting from camping opportunities <br />which depend on open bars for good views, fewer insects, and ease of access to the river), loss of sloughs and the <br />filling of pools (both of which provide important habitat and good fishability for arctic grayling, the principal sport fish <br />on the river), and the increase in riffles, thus creating more critical reaches for navigation during low flow periods. <br />Readers should note that non - alluvial rivers, and even some alluvial rivers, may react somewhat differently than <br />is shown below. In fact, the Beaver Creek conclusions are hypothesized rather than observed changes (there has <br />been no decrease in flows on the river). The point is that there are a myriad of factors involved in how rivers adjust <br />to new flow regimes. These are simply descriptions of the common changes one might expect; the goal of an <br />instream flow assessment is to determine whether these will hold true as well as estimate the magnitude of them <br />for given decreases in flows. <br />many of the river's important natural features would be altered by sustained decreases in <br />flow. <br />25 <br />
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