2015
DOI: 10.1016/j.mechrescom.2015.02.008
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Breaking bore: Physical observations of roller characteristics

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Cited by 31 publications
(23 citation statements)
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References 17 publications
(12 reference statements)
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“…The same data set showed that the toe perimeter shape fluctuated rapidly with transverse distance and time, and large fluctuations in bore celerity were observed. That is, the celerity of the roller toe fluctuated rapidly with both time and transverse distance, although in a quasi-two-dimensional manner on average (Leng and Chanson 2015b). Yet both laboratory and field observations hinted to the existence of large-scale three-dimensional bubbly structures (Leng and Chanson 2015a, Chanson 2016, Leng and Chanson 2016.…”
Section: Tidal Boresmentioning
confidence: 99%
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“…The same data set showed that the toe perimeter shape fluctuated rapidly with transverse distance and time, and large fluctuations in bore celerity were observed. That is, the celerity of the roller toe fluctuated rapidly with both time and transverse distance, although in a quasi-two-dimensional manner on average (Leng and Chanson 2015b). Yet both laboratory and field observations hinted to the existence of large-scale three-dimensional bubbly structures (Leng and Chanson 2015a, Chanson 2016, Leng and Chanson 2016.…”
Section: Tidal Boresmentioning
confidence: 99%
“…It is believed that a more relevant analogy is the tidal breaking bore, as seen in Figure 2B. A breaking bore with a quasi-two-dimensional roller is observed for Froude numbers greater than 1.4 to 1.6 Chanson 2008, Leng andChanson 2015b), although localised form of breaking might appear for Froude numbers above 1.3 to 1.4, including shock waves upstream of and limited breaking at the first wave crest (Treske 1994, Chanson 2010a). In the field, tidal bores are typically observed for Froude numbers less than 2.5, as shown in Table 3.…”
Section: How Can Better Flow Analogies Help?mentioning
confidence: 99%
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“…In addition, the biochemical properties of the water may be considered particularly in natural estuarine systems, as well as the sediment characteristics. In tidal bores, a Froude similitude is derived theoretically (Henderson 1966, Lighthill 1978, Leng and Chanson 2015. That is, the model and prototype Froude numbers must be equal.…”
Section: Physical Modelling and Experimental Setup Presentationmentioning
confidence: 99%
“…where V 1 is the initial flow velocity positive downstream, U is the bore celerity positive upstream, g is the gravity acceleration, A 1 is the initial flow cross-section area and B 1 is the initial free-surface width (Leng and Chanson 2015). For Fr 1 < 1.3 to1.4, the bore is undular: its front is followed by a train of quasi-periodic free-surface undulations (Peregrine 1966, Treske 1994.…”
Section: Introductionmentioning
confidence: 99%