2017
DOI: 10.3390/land6030064
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Vegetation in Drylands: Effects on Wind Flow and Aeolian Sediment Transport

Abstract: Drylands are characterised by patchy vegetation, erodible surfaces and erosive aeolian processes. Empirical and modelling studies have shown that vegetation elements provide drag on the overlying airflow, thus affecting wind velocity profiles and altering erosive dynamics on desert surfaces. However, these dynamics are significantly complicated by a variety of factors, including turbulence, and vegetation porosity and pliability effects. This has resulted in some uncertainty about the effect of vegetation on s… Show more

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Cited by 48 publications
(47 citation statements)
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References 173 publications
(375 reference statements)
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“…Regardless, this small reduction in potential erosivity will likely be offset in many locations by vegetation responses to climate change. Wind erosivity depends on how the wind field interacts with exposed soil at the surface, which is controlled by vegetation cover and structure (Mayaud and Webb 2017). Vegetation both extracts momentum from the wind and provides shelter zones in which wind speeds at the surface are reduced depending on plant density and size (Wolfe and Nickling 1993).…”
Section: Figurementioning
confidence: 99%
“…Regardless, this small reduction in potential erosivity will likely be offset in many locations by vegetation responses to climate change. Wind erosivity depends on how the wind field interacts with exposed soil at the surface, which is controlled by vegetation cover and structure (Mayaud and Webb 2017). Vegetation both extracts momentum from the wind and provides shelter zones in which wind speeds at the surface are reduced depending on plant density and size (Wolfe and Nickling 1993).…”
Section: Figurementioning
confidence: 99%
“…5. Wind regime and sediment supply are known to control the formation of bare-sand dunes [20] largely. Changing coastlines around river mouths is a complex process.…”
Section: F Hydro Oceanographic Statementioning
confidence: 99%
“…The model provided insight into the effects of roughness elements on aeolian thresholds and fluxes with strong theoretical underpinning (Shao et al, 2015). Based on this, progress has been made in identifying other vegetation factors important to aeolian processes such as vegetation distribution (such as the 'telephone pole problem' by Okin, 2008), configuration (Brown, Nickling, & Gillies, 2008), porosity and pliability (Mayaud & Webb, 2017), and albedo (Chappell & Webb, 2016). The model considered frontal area of roughness elements to be the primary vegetation factor influencing aeolian processes, the model neglects some factors that affect the wind erosion process such as vegetation patterns, configuration, or lodging, which may be important for sediment flux (Webb, Okin, & Brown, 2014).…”
Section: Introductionmentioning
confidence: 99%