Exceptionally heavy rainfall affected the whole of Reunion Island from 27 February to 5 March 1993. The period was characterized by the persistent incursion of monsoonal northwesterlies down to the latitude of Reunion and by the presence of a powerful, stationary anticyclone south of the Mascarenes. The contact of these air masses formed an area of active convergence in which a weak, short-lived tropical depression developed. This instability in the southeasterly airstream generated particularly heavy rains on the steep eastern slopes of the Piton de la Fournaise massif through a classic orographic mechanism. A meteorological station located on the southeast windward slope of the Piton de la Fournaise massif at an altitude of 1600 m collected world record rainfall totals during this event. The rain was of “moderate” short-term intensity (0.5–4.5 mm min−1) but persisted for many days, exceeding local records on 2- to 8-h intervals and world records on 2- to 7-day intervals. A comparison with heavy rainfall events in 1994 and 1995, and a study of daily rainfall totals show the event was not unprecedented for Reunion Island and that the record-breaking rainfall totals were due, at least in part, to monitoring rainfall at a newly opened high-elevation location.
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Barcelo et al. (1997) studied this question.
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