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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 7 – Land Erodibility Dynamics 1980-2006assessed as be<strong>in</strong>g susceptible to w<strong>in</strong>d erosion, with >90% of the bioregion <strong>in</strong>dicated as be<strong>in</strong>gnot erodible.In the Channel Country, peaks <strong>in</strong> land erodibility occurred <strong>in</strong> similar periods to the MulgaLands. However, for every year <strong>in</strong> the period 1980-2006 >20% of the bioregion had at least alow to moderate susceptibility to w<strong>in</strong>d erosion. In no years did the model <strong>in</strong>dicate a nearcomplete(>90%) reduction <strong>in</strong> land erodibility. This consistently erodible condition is a resultof the aridity of the bioregion and its <strong>in</strong>herently low vegetation cover levels.Land erodibility <strong>in</strong> the Mitchell Grass Downs was generally low for the analysis period.Temporal changes <strong>in</strong> land erodibility <strong>in</strong> this bioregion are dist<strong>in</strong>ct <strong>in</strong> comparison to the otherregions. Peaks <strong>in</strong> erodible land occur at similar times to those <strong>in</strong> the Channel Country;however, the magnitudes of the peaks are not consistent. The portion of the Mitchell GrassDowns modelled as not be<strong>in</strong>g susceptible to w<strong>in</strong>d erosion did not drop below 75% between1993 and 2006.Extensive areas (>40%) of the Simpson-Strzelecki bioregion had some susceptibility to w<strong>in</strong>derosion <strong>in</strong> each year from 1980-2006. This high fractional cover is a result of the StrzeleckiDesert frequently hav<strong>in</strong>g moderate to high land erodibility. Figure 7.2 shows that theSimpson Desert dunefields did not experience regular high magnitude changes <strong>in</strong> erodibilitybetween 1980 and 2006. These dynamics are evident <strong>in</strong> the Strezelcki Desert and are<strong>in</strong>dicative of higher graz<strong>in</strong>g pressures, vegetation characteristics (dunefields populated withshort-lived grasses (Aristidia spp.) and forbs rather than drought-resistant hummock grasses(Triodia spp.)), and the higher sensitivity of the region to climate variability.Land Erodibility, Climate Oscillations and Ra<strong>in</strong>fallTable 7.1 summarises the correlations between annual ra<strong>in</strong>fall, the SOI, PDO and modellederodible land cover. There is a negative correlation between ra<strong>in</strong>fall and land erodibility (r 2 =-0.48, p

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