A severe thunderstorm affected Smithton, northwestern Tasmania, at 1700 UTC 21 November 1992, spawning an F3 tornado. The impact of the storm is described and its nature is assessed. The associated meteorological conditions are examined using conventional observations and modelled using a PC-based version of the operational Australian numerical weather prediction model, RASP. Model experiments suggest that the Tasmanian topography affected the location and, in some areas, the strength of atmospheric vertical motions during this event.
Fox‐Hughes et al. (Sun,) studied this question.
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