Analysis uncovers storm formation in northern Bass Strait, suggesting new forecasting approaches.
The formation of the severe storm of 5th August 1959 in northern Bass Strait is discussed briefly. Although characteristically a secondary depression, it does not fit into an earlier classification. Correspondence between its appearance and the super-imposition of positive vorticity advection over a low level front is claimed. While it is difficult to forecast the former, analysis of the westerlies from the oceanic data may resolve the whereabouts of a front. If one is predicted to be in a favourable position for further development, the first requirement - an alert - is satisfied.
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J.C. Langford (1960) studied this question.
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