Analysis indicates that surface circulation indices signal the persistence of large troughs in Australia, suggesting future weather trends.
Indices of the westerly. surface circulation from 35-50°S and 40-175°E were plotted as running five day means, as allso that at the 300 mb level, over the Australian area from 115-165°E; for the latter, the mean strength of the jet stream was used as an index. Peak values of both indices were found to coincide with the occurrence of a large quasi stationary trough south of the Continent.
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D. S. Wright (1958) studied this question.
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