Flow dynamics over a foredune scarp. Issue 5 (14th January 2019)

• Record Type: Journal Article
• Authors: Piscioneri, Ned; Smyth, Thomas A.G.; Hesp, Patrick A.
• Is Part Of: Earth surface processes and landforms. Volume 44:Issue 5(2019)
• Page Start: 1064
• Page End: 1076
• Publication Date: 2019-01-14
• Subjects: scarp -- foredune -- wind flow -- turbulence -- helicoidal flow; Geomorphology -- Periodicals; 551.4
• DOI: 10.1002/esp.4555
• Languages: English
• ISSNs: 0197-9337

Abstract

Abstract: The nature of wind flow over a small, 0.6 m high foredune scarp is investigated on the Sir Richard Peninsula, South Australia during a variety of incident wind directions and speeds. The study provides additional supporting evidence that the presence of the scarp and the dune exerts a strong influence on a landwards trending reduction in wind velocity and an increase in turbulence, with the greatest area of turbulence occurring near and at the foredune scarp base. For an incident oblique wind, an alongshore helicoidal flow is formed within a separation region along the scarp basal region. In this region, the coefficient of variation (CV) of wind speed is high and displays significant fluctuations. The flow at the scarp crest is compressed, streamlined and accelerated, turbulence is suppressed, and local jets may occur depending on the incident wind approach angle. Jets are more likely where the incident flow is perpendicular or nearly so. A flow separation region does not develop downwind of the scarp crest where the morphology of the foredune stoss slope downwind of the scarp is more convex (as in this case) rather than relatively flat, and possibly due to the presence of vegetation at the scarp crest. A tentative model of the flow regions developed across a backshore–scarp–foredune region during oblique incident flow is provided. © 2018 John Wiley & Sons, Ltd. Abstract : The dynamics of wind flow over a small, 0.6 m high foredune scarp is investigated. For an incident oblique wind, an alongshore helicoidal flow is formed within a separation region along the scarp basal region. The flow at the scarp crest is compressed, streamlined and accelerated, turbulence is suppressed, and local jets may occur.