Assessment of turbulence models for the simulation of turbulent flows past bluff bodies
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...…jets as seen just seaward of the scarp crest (2D-4) and on the foredune stoss slope (2D-6) are common near, and at the crest of steep cliffs and scarps and also over high foredunes (Hsu, 1977; Hesp et al., 2009; Yasin and Al-Harbi, 2013; Pires et al., 2015; Elkhoury, 2016; Hesp and Smyth, 2016)....
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...Such jets as seen just seaward of the scarp crest (2D-4) and on the foredune stoss slope (2D-6) are common near, and at the crest of steep cliffs and scarps and also over high foredunes (Hsu, 1977; Hesp et al., 2009; Yasin and Al-Harbi, 2013; Pires et al., 2015; Elkhoury, 2016; Hesp and Smyth, 2016)....
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...If the morphology of the dune (or other topography) is flat to relatively flat downwind of the scarp crest, flow separation usually occurs and a region of turbulent reversing flow develops (Wilhelm et al., 2003; Largeau and Moriniere, 2007; Pires et al., 2015; Rowcroft et al., 2015; Elkhoury, 2016)....
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...…where the crest is around 90° to the scarp wall, and unvegetated, there is typically a region of separated reversing flow (see multiple studies reviewed in Bowen and Lindley, 1974, 1977; Hattori and Nagano, 2010; and Elkhoury, 2016), but this separation zone does not appear to occur at this site....
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...This is due to the high vertical acceleration of flow up, and then over the scarp crest as observed in Figure 7, and in many other studies (Rowcroft et al., 2014; Elkhoury, 2016)....
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