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The cultivated steppe region constitutes the principal wheat zone; agriculture is intensively pursued along the banks of the rivers.
Given the high spatial environmental variability within the Australian wheat zone the remarkable level of agreement between results from these two methodologies provides evidence of the robustness of the GYGA protocols.
The fifteen year average Ya and Yw values for each of the 245 statistical local areas (SLAs) in Australia's wheat zone were strongly and positively correlated (Ya = 0.456 x Yw + 0.15; R2 = 0.65; RMSE = 0.291; p < 0.001) such that the yield gap (Yw-Ya) tended to be larger in SLAs with higher Yw values.
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In the winter wheat zones III, IV, V and IX, the frequency of Hap-6B-3 was highest, whereas in spring wheat zones VI and X, Hap-6B-2 was more frequent, and Hap-6B-1 was relatively frequent only in zone VII.
Modifying farms in the wheat-sheep zone to meet the guidelines is technically feasible, but not economically attractive at present.
While production landscapes in the pastoral and high rainfall zones of Australia could potentially meet most of these guidelines, very few in the wheat-sheep zone do.
The wheat-sheep zone has a climate and topography that generally allows regular cropping of grains in addition to the grazing of sheep and cattle on a more intensive basis than in the pastoral zone.
At Narrogin (wheat-sheep zone) there is almost no summer moisture and growth occurs mainly in autumn and spring although the temperature limitations in winter are not as severe as those at Hamilton.
The empire was broadly divided into rice zones and wheat and millet zones.
There were numerous reports of "legume decline " covering Trifolium subterraneum, Medicago species and Trifolium repens in both the high-rainfall and wheat-sheep zones.
In the high rainfall and wheat-sheep zones, low nutritive value of herbage over the summer dry season and low herbage availability in the autumn and winter are important limitations to animal production (Wilson and Simpson, 1993).
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