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Cyclone Mahina

Australian region cyclone in 1899

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Through Pascal (unit)

While the Australian Bureau of Meteorology, which is the Regional Specialised Meteorological Centre of the basin, estimates Mahina's peak central pressure to be 914 hPa (26.99 inHg), the World Meteorological Organization is currently considering an application from Queensland scientists and researchers to have this value upgraded to 880 hPa (25.99 inHg), based on data from post-storm analysis. This would officially make Mahina the most intense cyclone recorded to have hit the Australian mainland, and the most intense tropical cyclone recorded making landfall anywhere in the world, as well as the most intense tropical cyclone ever recorded in the Southern Hemisphere, a title currently held by Cyclone Winston. Cyclone Mahina produced a 9-metre-high (30-foot) surge.

Impact

Tropical Cyclone Mahina struck Australia on 4 March 1899, with a likely minimum central pressure of 880 hectopascals (26 inHg). Mahina ranks among the most intense cyclones ever observed in the Southern Hemisphere and almost certainly as the most intense cyclone ever observed off the Eastern states of Australia in recorded history. Clement Lindley Wragge, Government Meteorologist for Queensland, pioneered the naming of such storms and gave this storm its name, Mahina.

Storms of such intensity occur extremely rarely. Scientists identified two other Category 4 or 5 super-cyclones that struck Australia, in the first half of the 19th century, from their effects on the Great Barrier Reef and the Gulf of Carpentaria. This same research shows that on average, such super-cyclones occur in the region only once every two or three centuries.

A pearling fleet, based at Thursday Island, Queensland, was anchored in or near the bay before the storm. Within an hour, the storm drove much of the fleet ashore or onto the Great Barrier Reef; other vessels sank at their anchorages. Four schooners and the manned Channel Rock lightship were lost. A further two schooners were wrecked but later re-floated. The fleets lost 54 luggers, and a further 12 were wrecked but re-floated. People later rescued more than 30 survivors of the wrecked vessels from the shore; however, the storm killed more than 400 people, mostly non-European immigrant crew members. A depiction of the schooner Crest of the Wave in the storm was later sketched in a painting.

A large storm surge, reportedly 13 metres (43 ft) high, swept across Princess Charlotte Bay and then inland about 5 kilometres (3.1 mi), destroying anything left of the Bathurst Bay pearling fleet and the settlement.

An eyewitness, constable J. M. Kenny, reported that a 48-foot (15 m) storm surge swept over their camp at Barrow Point atop a 40-foot (12 m)-high ridge and reached 3 miles (4.8 km) inland, the largest storm surge ever recorded. However, reviewing the evidence for this surge, some scientists modeled a surge only 2 metres (6 ft 7 in) to 3 metres (9.8 ft) in height, based on the official 914-hectopascal (27.0 inHg) central pressure. They also surveyed the area, seeking wave-cut escarpments and deposits characteristic of storm events, but found none higher than 5 metres (16 ft). Of the 48-foot (15 m) surge, they suggested an incorrectly cited ground level or an involvement of freshwater (rain) flooding. A later study considers this conclusion likely premature and questions the barometer reading as unreliable and not representative of the actual lowest pressure. This subsequent study also examined new evidence of exceptionally high storm surge and inundation.

The cyclone continued southwest over Cape York Peninsula, emerging over the Gulf of Carpentaria, before doubling back and dissipating on 10 March.

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