4.5 Article

Skimming Flow and Sand Transport Within and Above Ammophila (Marram) Grass on a Foredune

Journal

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2023JF007143

Keywords

foredune; skimming flow; suspended and modified saltation; aeolian transport; Ammophila

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This study investigates wind flow and sand transport over a foredune dominated by Ammophila grass with different densities on the Leba barrier in Poland. High resolution data is provided on saltation and suspended sand transport under both canopy and skimming flow conditions. The study reveals that the sand concentration decreases with height and reaches a minimum at different elevations depending on Ammophila grass density. The results also show that the maximum sand transport increases with vegetation density and more sand is transported at higher elevations above the canopy surface than above a bare sand surface in skimming flow.
An investigation of wind flow and sand transport over a low to high density Ammophila dominated foredune on the Leba barrier, Poland, utilizing multiple anemometers and sand traps is presented. The study provides the first high resolution data on modified saltation and suspended sand transport over a foredune under conditions of both canopy and skimming flow. Topographic acceleration of flow and topographic steering over the foredune were observed during oblique incident above threshold flow conditions. The concentration of sand in aeolian transport decreases with height to a minimum that is reached at different elevations above the ground, depending on Ammophila grass density. Of the three Ammophila (marram) grass densities investigated, nearly half (46%) of the total sand-transport rate occurred above the lower density Ammophila grass, whereas up to 70% of the total transport occurred above the higher density marram grass. This likely results from both elastic collisions of sand grains with grass leaves over the Ammophila canopy and the different positions of the canopy rebounding surface, which is sensitive to even slight changes in wind speed. In addition, as plant density increases, there is less flow penetration into the canopy, vegetative forcing (similar to topographic forcing) of vertical flow is greater, and sand in both modified saltation and suspension is forced higher above the canopy in skimming flow. The maximum sand transport above the vegetation canopy increased in elevation from 32 to 48 to 53 cm as the vegetation density increased from low to moderate to high, respectively. The study also demonstrates that in skimming flow, relatively more sand is transported at higher elevations above a canopy surface than above a bare sand surface.

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