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Cyclone Tessi

Category 3 Australian region cyclone in 2000

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Through Landslide and High-pressure area

Tessi's strong winds caused widespread damage along the coast from Ingham to Ayr, most notably around Townsville, where many trees were uprooted and 50,000 homes lost electricity. Buildings and vehicles were damaged by the winds and fallen trees, and roadways surrounding the city became impassable. Torrential rains, amounting to 423.4 mm (16.67 in) in just 24 hours, saturated a hillside in Castle Hill and caused a large landslide. Hundreds of Castle Hill residents were forced to leave their homes, and many structures were inundated with mud and debris. The landslide dislodged a large boulder uphill from several residences, creating a period of local concern before workers stabilised the slope. Along the coast, the storm wrecked boats and eroded beaches. Total damage in Townsville was estimated to be at least $50 million (2000 AUD), and the name Tessi was later retired due to the cyclone's impacts.

Meteorological history

Cyclone Tessi originated in a northwest–southeast oriented trough of low pressure that developed in the Coral Sea at the end of March 2000. Similar conditions would lead to the genesis of Cyclone Vaughan in the same region just days later. Initially forming within the trade winds east of an upper-level trough over eastern Australia, the disturbance that ultimately spawned Tessi persisted in the area for nearly a week before becoming associated with an organised area of convection on 31 March, about 1,100 km (680 mi) east of Cooktown, Queensland. At that point, the Bureau of Meteorology's (BoM) Tropical Cyclone Warning Centre in Brisbane operationally identified the system as a tropical low and began issuing gale warnings. At 00:00 UTC on 2 April, the Joint Typhoon Warning Center (JTWC) designated the system 22S. Diffluence from an anticyclone to the east promoted favourable outflow in the upper levels of the atmosphere, and a closed centre of circulation rapidly formed. As the disturbance tracked southwestward around the periphery of a mid-level ridge to the south, its appearance on satellite imagery continued to improve, with distinct rainbands wrapping around the centre. At 18:00 UTC on 1 April, the system intensified into Tropical Cyclone Tessi while located under 500 km (310 mi) northeast of Townsville, Queensland.

Tessi was an extremely small tropical system, described as a "midget cyclone," that continued to contract due to rising environmental air pressures as it approached the coast. Additionally, the storm's wind field was lopsided, with gale-force winds extending 185 km (115 mi) to the south of the centre but only 30 km (19 mi) to the north. Nonetheless, the parent trough provided an area of generally weak inhibiting wind shear, allowing the cyclone to quickly strengthen. Around 18:00 UTC on 2 April, while Tessi was just offshore, a small eye feature only 10 km (6.2 mi) across became evident on weather radar. By 20:00 UTC, the storm reached its peak intensity with 10-minute maximum sustained winds of 140 km/h (85 mph) and a minimum central air pressure of 980 mbar (28.94 inHg). This made it a Category 3 severe tropical cyclone on the Australian cyclone scale. The JTWC estimated weaker 1-minute winds of 95 km/h (60 mph). Shortly after peaking, Tessi made landfall just south of Lucinda, or about 75 km (45 mi) northwest of Townsville. Land-based observations and radar imagery suggested that the storm was more intense than indicated by its satellite presentation. Upon moving ashore, the cyclone slowed and rapidly deteriorated, and it dissipated by 00:60 UTC on 3 April. The small cyclone's rapid strengthening before landfall was generally not well-forecast by weather models; in particular, the ECMWF model anticipated that the system would degenerate back into an open trough before moving ashore.

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