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Wind Erosion in Western Queensland Australia

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

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Chapter 3 – Modell<strong>in</strong>g Land Erodibility Review3.2.5 <strong>W<strong>in</strong>d</strong> <strong>Erosion</strong> Stochastic Simulator (WESS)The <strong>W<strong>in</strong>d</strong> <strong>Erosion</strong> Stochastic Simulator (WESS) is the w<strong>in</strong>d erosion module of the EPIC(Environmental Policy Integrated Climate) erosion model (Van Pelt et al., 2004). WESS is aprocess-based model that predicts w<strong>in</strong>d erosion on an event or periodic basis. The modelprovides assessments of soil loss at user-specified distances with<strong>in</strong> <strong>in</strong>dividual fields. Themodel uses <strong>in</strong>puts of soil surface data <strong>in</strong>clud<strong>in</strong>g texture, soil surface moisture and dry<strong>in</strong>g rate,erodible soil thickness, surface soil bulk density, and soil roughness parameters for largeaggregates (random roughness), and ridge height and spac<strong>in</strong>g (oriented roughness). This iscoupled with local w<strong>in</strong>d speed data and a stochastic w<strong>in</strong>d speed perturbation factor tosimulate dust emission (Potter et al., 1998). WESS simulates w<strong>in</strong>d erosion based on dailyw<strong>in</strong>d speed distributions adjusted by soil, surface roughness, vegetation cover and erod<strong>in</strong>gfield length factors:YW= ( FI )( FR)( FV )( FD)!t0YWRdtWL(3.14)where YW is the w<strong>in</strong>d erosion estimate (kgm -2 ), YWR is the erosion rate (kgm -1 s -1 ), WL is theunsheltered field length (m), FI is the soil erodibility factor, FR is the surface roughnessfactor, FV is the vegetation cover factor, FD is the field length factor (based on WL), and t isthe duration of w<strong>in</strong>d greater than a threshold velocity. YWR is calculated us<strong>in</strong>g the approachof Skidmore (1986). The soil erodibility adjustment factor is based on the static <strong>W<strong>in</strong>d</strong>Erodibility Groups (WEGs) reported by Woodruff and Siddoway (1965), and used <strong>in</strong> theWEQ model:( 0.0001 )IFI = *exp * YW695(3.15)where I is the soil erodibility factor (tha -1 ) with values assigned by soil texture and theWEGs. The effect of oriented surface (cultivated ridge) roughness (FR) is calculated as afunction of w<strong>in</strong>d direction, and the impact angles of saltat<strong>in</strong>g gra<strong>in</strong>s:RFC FR = 1 exp (3.16) RFB 80

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