Sandy Beach Morphodynamics 2020
DOI: 10.1016/b978-0-08-102927-5.00011-4
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Rip currents

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Cited by 8 publications
(4 citation statements)
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“…During the most energetic events, it is possible to observe localized ruptures in the embayments of the inner and outer bars (Figure 14), creating channels that incise the crest of the bar and allowing for the expulsion of rip currents [95,[107][108][109]. The latter is more frequent on the inner bar (35% of observations; Figure 14) than on the outer bar (5% of observations; Figure 14) and may give rise to asymmetrical inner bars, confirming that oblique waves are required for their formation [8,110,111].…”
Section: Development and Evolution Of Rip Channelsmentioning
confidence: 83%
“…During the most energetic events, it is possible to observe localized ruptures in the embayments of the inner and outer bars (Figure 14), creating channels that incise the crest of the bar and allowing for the expulsion of rip currents [95,[107][108][109]. The latter is more frequent on the inner bar (35% of observations; Figure 14) than on the outer bar (5% of observations; Figure 14) and may give rise to asymmetrical inner bars, confirming that oblique waves are required for their formation [8,110,111].…”
Section: Development and Evolution Of Rip Channelsmentioning
confidence: 83%
“…Surf-related drownings in the region tend to be associated with rough surf and rip currents at headlands groins and jetties. While most rips in the region are structural (see Houser, 2020 ), there is evidence of bathymetrically controlled rips resulting from transverse bar and rip nearshore morphology on some beaches ( Vlodarchyk et al, 2019 ).…”
Section: Study Sitementioning
confidence: 99%
“…Numerical studies examining flow and bathymetry interactions have focused on predicting rip spacing (Calvete, 2005; Damgaard et al., 2002; Deigaard et al., 1999; Reniers et al., 2004; Valipour & Bidokhti, 2018), and the dependence of rip currents on channel dimensions (Brander, 1999; Castelle et al., 2010; Hong et al., 2021; Kennedy et al., 2008; McCarroll et al., 2018; Winter 2012). However, the bathymetric effects on rip generation and strength remain uncertain, and there are few field and corresponding numerical investigations of sediment transport and channel evolution (Houser et al., 2020).…”
Section: Introductionmentioning
confidence: 99%
“…Channel rips are strong, wave‐driven offshore‐directed surfzone currents associated with alongshore bathymetric variability. Rip current strengths typically are of the order of 0.5 m/s, but can exceed 2 m/s during storms (Houser et al., 2020), and pose a major risk for beachgoers (Brander, 2015). In addition, rips are important for the exchange of sediments, nutrients, pollutants, phytoplankton, and fish larvae across the surf zone (Aagaard et al., 1997; Brown et al., 2009, 2015; Fujimura et al., 2014; Gallop et al., 2018; MacMahan et al., 2010; Reniers et al., 2009).…”
Section: Introductionmentioning
confidence: 99%