2010
DOI: 10.1002/rra.1324
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Determining the effects of dams on subdaily variation in river flows at a whole‐basin scale

Abstract: River regulation can alter the frequency and magnitude of subdaily flow variations causing major impacts on ecological structure and function. We developed an approach to quantify subdaily flow variation for multiple sites across a large watershed to assess the potential impacts of different dam operations (flood control, run-of-river hydropower and peaking hydropower) on natural communities. We used hourly flow data over a 9-year period from 30 stream gages throughout the Connecticut River basin to calculate … Show more

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Cited by 90 publications
(95 citation statements)
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References 37 publications
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“…In response, several indexes for measuring the hourly fluctuation have been proposed in the last decade [35][36][37]. The Richard-Baker (R-B) index [35] for flow flashiness is one that has found numerous applications in the last five years [5,6,12,38,39]:…”
Section: Sub-daily Hydrologic Alterationmentioning
confidence: 99%
“…In response, several indexes for measuring the hourly fluctuation have been proposed in the last decade [35][36][37]. The Richard-Baker (R-B) index [35] for flow flashiness is one that has found numerous applications in the last five years [5,6,12,38,39]:…”
Section: Sub-daily Hydrologic Alterationmentioning
confidence: 99%
“…The simplest one was the comparison between the regulated and unregulated sites. Zimmerman et al (2010) determined the effects of dams on sub-daily variation in river flows for multiple sites across a large watershed by this method. Magilligan and Nislow (2005) assessed hydrological changes associated with dams by a hydrological model, supplemented with orientation statistics for some hydrograph parameters.…”
Section: Introductionmentioning
confidence: 99%
“…This category contains a sort of difference pattern, such as difference between adjacent ordinates, difference between ordinate and its mean. The second category is called the divided category, and it includes the FOD divided by the maximum [17], SD divided by the mean [13,14,18], coefficient of variation [19], normalized SD [20], and Richards-Baker Flashiness (RBF) index [5,19,[21][22][23][24]. The third is the distribution, and contains the distribution of the FOD [4] and the distribution of exceedance [6].…”
Section: Introductionmentioning
confidence: 99%
“…The RBF, based on Indicators of Hydrological Alteration (IHA) [25] and Richards Pathlength (RP) [26], was proposed by Baker and Richards in 2004 [27] and has subsequently been widely used to describe stream flow fluctuations [5,19,[21][22][23][24]. Due to ignorance of contour variation of process, the FOD, SD and RBF are capable of describing the dispersion of process but inadequate to discern the contour difference.…”
Section: Introductionmentioning
confidence: 99%