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Cyclone Althea

1971 natural disaster in Australia

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Through Pascal (unit) and High-pressure area

While moving ashore, Althea generated wind gusts as high as 215 km/h (134 mph) that wrought significant destruction around Townsville and left nearby Magnetic Island in a state of ruin; almost all of the buildings on the island were damaged to some degree. A significant 3.66 m (12.0 ft) storm surge battered the mainland, while high waves destroyed roads and seawalls. Beaches receded by up to 15.8 m (52 ft) due to coastal erosion. In Townsville, thousands of homes were damaged and many were destroyed. The most widespread damage was to roofs, which were often poorly or not at all secured. The damage from Althea prompted Queensland to develop its first statewide building codes, requiring new homes to be cyclone-resistant. Townsville was the first community to adopt the enhanced construction standards. In addition to the coastal effects, Althea triggered extensive river flooding in interior Queensland. Most major roads in western portions of the state were cut off by floodwaters, and hundreds of families had to leave their homes for higher ground. In the aftermath of the cyclone, 600 Australian Army soldiers aided recovery efforts in Townsville and Magnetic Island, while both state and federal governments contributed disaster relief funds. Three people were killed and damage totaled $120 million (1971 AUD).

Meteorological history

Cyclone Althea originated in an expanding area of thunderstorm activity near the Solomon Islands in mid-December 1971. Although little is known about the storm's genesis because of sparse reports and infrequent weather satellite images, the disturbance is thought to have organised into a tropical low on 19 December as it tracked slowly southwestward into the Coral Sea. According to the Bureau of Meteorology's (BoM) Tropical Cyclone Warning Centre (TCWC) in Brisbane, the system reached tropical cyclone status around 06:00 UTC on 20 December, less than 300 km (200 mi) southwest of Honiara. Just after 23:00 UTC on 21 December, imagery from the United States ESSA-8 satellite showed the first indications of an emerging eye feature. Althea tracked southwest toward the coast of Queensland around a subtropical ridge to the south, and steadily strengthened. Near 18:00 UTC on 22 December, it reached its peak intensity with 10-minute maximum sustained winds of 130 km/h (80 mph); this made it a Category 3 severe tropical cyclone on the Australian scale. The cyclone's central barometric pressure of 952 hPa (28.1 inHg) was estimated using the lowest recorded air pressure, 971.5 hPa (28.69 inHg) at Townsville Airport, a 32 km (20 mi) radius of maximum wind, and environmental air pressures.

Late on 22 December, the eye remained obscured to satellite imagery by a canopy of cirrus clouds while the cyclone passed north of Lihou Reef. Early the next day, it tracked just south of the automated weather station on Flinders Reef. Althea likely continued to organise until landfall, which occurred at 23:00 UTC on 23 December – 09:00 AEST on Christmas Eve – near Rollingstone, about 50 km (30 mi) north of Townsville. The landfall point placed Townsville and nearby Magnetic Island in the cyclone's powerful left-front quadrant. Because of the tight pressure gradient between Althea and the high pressure area to the south, gale-force winds extended well to the south of the cyclone's centre. While the system was moving ashore, land-based radar imagery identified an ongoing eyewall replacement cycle, with two distinct, concentric eyewalls – rings of intense thunderstorms surrounding the centre. The strongest winds were found under the contracting outer ring, which shrank from 55 to 39 km (34 to 24 mi) between 21:00 and 23:00 UTC to become the dominant eyewall as the inner ring dissipated. Consequently, extreme winds initially extended relatively far from the centre.

The storm quickly weakened as it continued southwest, passing just north of Charters Towers City, though it continued to produce heavy rainfall over interior Queensland. Curving southeastward, Althea re-emerged over open waters between Maryborough and Double Island Point on 26 December and began to intensify once again. At 00:00 UTC on 28 December, the cyclone reached a third peak with 10-minute winds of 110 km/h (70 mph), but as it turned more toward the south, increasingly cooler sea surface temperatures weakened the cyclone. On 29 December, Althea lost its tropical characteristics over the Tasman Sea.

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