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1 Spatial Modelling of the Terrestrial Environment - Georeferencial

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<strong>Modelling</strong> Wind Erosion and Dust Emission on Vegetated Surfaces 145<br />

Table 7.3<br />

SWEMO input parameters for soils <strong>of</strong> <strong>the</strong> Jornada Basin<br />

Texture Sandy loam Loamy sand Clay loam Gravelly sand<br />

u ∗ts (cm s −1 ) 29 34 68 28<br />

Log(F a /Q tot (cm −1 )) −3.7 −4.5 −5.7 −5.7<br />

A 1.0 1.0 1.0 1.0<br />

<strong>Spatial</strong>ly-Explicit Wind Erosion and Dust Flux Model<br />

(SWEMO)<br />

Vegetation<br />

Map<br />

Soil<br />

Map<br />

Wind speed data<br />

Reproject to<br />

soil map projection<br />

Create histogram<br />

wind speed<br />

Parameter lookup<br />

file containing info<br />

on each plant community<br />

Parameter lookup<br />

file containing info<br />

on each soil type<br />

Create maps <strong>of</strong>:<br />

U *ts , Z 0 , A, σ,<br />

β, λ, & F a /Q tot<br />

Calculate histogram <strong>of</strong><br />

Derive map <strong>of</strong> U *t<br />

U * for each cell<br />

Calculate<br />

Q tot for each cell<br />

Calculate F a for<br />

each cell<br />

Figure 7.3<br />

(SWEMO)<br />

Processing stream for <strong>the</strong> spatially explicit wind erosion and dust flux model<br />

disturbance, a road, a dry river or a dry lake, may account for <strong>the</strong> majority <strong>of</strong> dust emitted<br />

in an area, but be insignificant on <strong>the</strong> scale at which most maps are produced.<br />

In <strong>the</strong> present study, a site with all requisite data (soil maps, vegetation maps, wind data<br />

and a wealth <strong>of</strong> ongoing ecological research) was chosen to test SWEMO. The Jornada

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