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Cyclone Dinah

Category 4 South Pacific and Australian region cyclone in 1967

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Through Atmospheric pressure and Jet stream

According to a study, Dinah caused the largest waves observed in southern Queensland in centuries. The system also inflicted extensive damage on Heron Island during its passage to the southern part of the state, starting with the flooding of massive north-easterly swellings and a day later with heavy winds. Although Dinah remained offshore, its outer rainbands caused heavy rains and gusty winds that uprooted trees, starting from Rockhampton Region to Grafton in New South Wales. Some residential institutions lost their roofs due to the wind, while banana and sugarcane crops were destroyed and inundated by floodwaters. Severe erosions were reported in Emu Park and Maryborough-Bundaberg areas. Massive rainfall amounts were recorded in some parts of Queensland, New South Wales and New Zealand's North Island as the extratropical remnant. Storm surges were also seen on Sunshine Coast, Queensland. Tourists on Lord Howe Island were stranded by the storm, while many residents had to be rescued on different beaches due to large swells. A man in North Island in New Zealand was feared drowned due to Dinah, while another was missing due to his car being submerged in floods. The damage was described as severe, but the numerical amounts were unknown.

Meteorological history

Dinah was first noted as a tropical low on 23:00 UTC on 22 January in the adjacent South Pacific basin, nearly 168 kilometers to the south-southwest of Lata, Solomon Islands. In the early stages of its life, the disturbance moved west-southwestwards while remaining weak, possibly due to its unfavorable environment. More recent study about the track of the storm showed that the precursor to Dinah developed on 08:00 UTC that day, north-northwest of Vanuatu. Over the next hours, the system moved southwestwards while becoming organized; however, the observations of the low remained scarce due to the lack of weather stations in the area. The best track of the storm from the Joint Typhoon Warning Centre revealed that the agency started to monitor the developing system in their Significant Tropical Weather Outlooks on 12:00 UTC on 22 January, estimating the wind speeds of the system to be at 15 knots. Nevertheless, the disturbance organised further and on 24 January, the organisation of the low became enough for the Bureau of Meteorology's (BoM) Tropical Cyclone Warning Centre in Brisbane to name the system Dinah as it entered the Area of Responsibility (AoR) of Queensland's capital. Two days later, the JTWC upgraded the system to a tropical storm on the modern-day Saffir–Simpson scale. Under the warm waters of the Coral Sea, Dinah started to slowly intensify, although its motion slowed down again. At 11:00 UTC of 25 January, the Brisbane TCWC upgraded the system to a Category 2 tropical cyclone as Dinah's eye started to emerge. Continuing its southwestward motion, Dinah continued to strengthen, as conditions in the Coral Bay favored the system to organize. At 23:00 UTC on 26 January, the TCWC Brisbane further upgraded the system to a Category 3 severe tropical cyclone, as its eye became well-defined and the system became more compact in size, while located nearly 612 kilometers to the east-northeast of Bowen, Queensland. Dinah began to curve south-southwestwards, approaching the southern coasts of Queensland while reaching its peak intensity of 195 km/h (121 mph), making it a Category 4 severe tropical cyclone. The cyclone then brushed the southern portion of the Great Barrier Reef, starting from Halfmoon Reef on 27 January and Gater Reef, Sweetlip Reef and the Hixson Reefs on 28 January before exiting the area. On the next day, while nearing the coast of Queensland, it made landfall on Fraser Island between 05:00 and 06:30 UTC that day, first on Sandy Cape where its lighthouse recorded a barometric pressure of 944.8 hPa (27.9 inHg), being the lowest known pressure of Dinah. It turned south-southeastwards, reemerging on the Coral Bay before making a second landfall, west of Waddy Point that day before moving on to the said bay, before slowing down again for the third time. The eye of Dinah became cloud-filled as it moved away from the coast of Queensland, although it remained in that intensity until it was downgraded to a Category 3 severe tropical cyclone at 11:00 UTC on 30 January. Further weakening took place as Dinah started to enter an unfavorable environment and 12 hours later, Dinah became a Category 2 tropical cyclone as it passed near Lord Howe Island before undergoing extratropical transition as it interacted with the jet stream. It then fully became extratropical on the next day, on the Tasman Sea. Ex-Dinah then brushed North Island on 2 February before emerging on the South Pacific Ocean by the next day, where it dissipated.

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