Abstract
A five-winter satellite study of the ‘instant occlusion" mode of extratropical cyclogenesis has been undertaken for the Southern Hemisphere oceans. The phenomenon shows a maximum frequency of occurrence over latitudes 30–55°S, where it is closely associated with the locations of the winter “climatic fronts” The longitudes of Australasia and the eastern Indian Ocean are particularly favored for "instant occlusion” developments. Month-to-month variations in the frequency of their occurrence are relatedtothebemispheric-scale changes in total cyclonic vortex activity observed during the winter season.

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