2014
DOI: 10.1016/j.jhydrol.2014.07.015
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Using regional flow classes as references to analyse flow regime anomalies across a set of regulated Canadian rivers

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Cited by 10 publications
(20 citation statements)
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“…All flow indices described by McLaughlin et al . (), in addition to those created to capture hourly variations in the flow record (Zimmerman et al ., ; Macnaughton et al ., ), were calculated for each of the rivers surveyed for a total of 211 flow indices. Flow indices expressed as discharge units (volume per time) were normalised by dividing these indices by the median flow (daily or hourly as appropriate) for the available flow records (McManamay et al ., ).…”
Section: Methodsmentioning
confidence: 99%
“…All flow indices described by McLaughlin et al . (), in addition to those created to capture hourly variations in the flow record (Zimmerman et al ., ; Macnaughton et al ., ), were calculated for each of the rivers surveyed for a total of 211 flow indices. Flow indices expressed as discharge units (volume per time) were normalised by dividing these indices by the median flow (daily or hourly as appropriate) for the available flow records (McManamay et al ., ).…”
Section: Methodsmentioning
confidence: 99%
“…Hydro‐peaking type systems were defined as exhibiting frequent periods of significant hourly or diel hydrologic fluctuations over a year caused by rapid opening and closing of reservoir release structures (Cushman, ; Flodmark et al , ). Precise, quantitative thresholds distinguishing these regulation types are not internationally accepted, so we assigned ‘types’ to our rivers based on preliminary analyses of the regulated hydrographs (after McLaughlin et al , ).…”
Section: Methodsmentioning
confidence: 99%
“…Flow regime is typically described using hydrological indices representing five flow components (i.e., magnitude, frequency, duration, timing, and rate of change; Poff et al 1997) that can be quantified at various temporal scales (Richter et al 1996;Poff et al 1997;Zimmerman et al 2010). Hydrological indices are used for classifying rivers (Poff and Allan 1995;McMahon et al 2007;McLaughlin et al 2014), measuring flow alteration (Richter et al 1996;Nislow et al 2002;Mathews and Richter 2007;Macnaughton et al 2015), and assessing the influence of flow regime on ecological processes and community attributes (Poff and Allan 1995;Kennard et al 2010). For instance, short-term variation of flow can cause fish stranding mortality (Cushman 1985;Bradford et al 1995;Young et al 2011) and downstream displacement (Jeffries et al 2005).…”
Section: Introductionmentioning
confidence: 99%
“…For example, hydropower generation can be achieved by using run-of-the-river (ROR), storage, or peaking facilities, each of which potentially poses a different suite of effects on specific hydrological indices and fish community attributes in river segments downstream from such facilities (McLaughlin et al 2014). ROR facilities typically consist of a small reservoir where water freely flows through turbines generally producing little or no effects on the downstream flow regime (Bratrich et al 2004).…”
Section: Introductionmentioning
confidence: 99%
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