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Wind Erosion in Western Queensland Australia

Modelling Land Susceptibility to Wind Erosion in Western ... - Ninti One

Modelling Land Susceptibility to Wind Erosion in Western ... - Ninti One

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Chapter 1 - Introduction• The ability of soils to susta<strong>in</strong> vegetation and livestock decreases;• Agricultural and pastoral productivity decreases;• Nutrient enrichment of streams occurs with the <strong>in</strong>flux of w<strong>in</strong>d blown sediments;• Spread of herbicides and pesticides off-farm; and• Damage to property (e.g. fences and roads) and farm <strong>in</strong>frastructure.Off-site effects of w<strong>in</strong>d erosion are relevant across scales and relate to the transport anddeposition of m<strong>in</strong>eral dust which (after Dentener et al., 1996; Prospero et al., 2002; Jickells etal., 2005 and others):• Alters the radiation balance <strong>in</strong> the atmosphere through scatter<strong>in</strong>g and absorption ofradiation;• Affects cloud nucleation and optical properties of the atmosphere;• Acts as a reactive m<strong>in</strong>eral species <strong>in</strong> the atmosphere;• Moderates the photochemical oxidant cycle and biogeochemical processes;• Acts as a source of Fe that may be metabolised by cyanobacteria and may subsequentlymoderate the nitrogen chemistry of the ocean;• Acts as a source of Fe that may be a limit<strong>in</strong>g nutrient for phytoplankton; and• Provides reaction sites for ozone and nitrogen molecules.Understand<strong>in</strong>g spatial and temporal variations <strong>in</strong> w<strong>in</strong>d erosion is required to develop methodsfor manag<strong>in</strong>g land degradation at the field (10 3 m 2 ) to landscape (10 3 km 2 ) scales, and forunderstand<strong>in</strong>g the regional to global scale consequences of dust transport. Surpris<strong>in</strong>gly littleattention has been given to the development of methods for assess<strong>in</strong>g spatio-temporalpatterns <strong>in</strong> land areas susceptible to w<strong>in</strong>d erosion.Exist<strong>in</strong>g maps of the location and extent of regions prone to w<strong>in</strong>d erosion are based on: fieldassessments of affected areas (Carter, 1985; Mezösi and Szatmári, 1998); observational dataon dust-storm frequencies (Goudie and Middleton, 2006); analyses of satellite imagery(Prospero et al., 2002; Wash<strong>in</strong>gton et al., 2003); and <strong>in</strong> a few cases spatial modell<strong>in</strong>g (Böhneret al., 2003; Coen et al., 2004). However, these methods for assess<strong>in</strong>g w<strong>in</strong>d erosion have anumber of limitations. These <strong>in</strong>clude:2

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