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Cyclone Zoe

2002 tropical cyclone

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Through Crop

Cyclone Zoe severely affected areas of Rotuma, the Solomon Islands, and Vanuatu. Heavy rainfall and strong winds were particularly disastrous to the Solomon Islands, especially on the islands of Anuta and Tikopia. There, numerous crops and fruit–bearing trees were destroyed. Beaches were also heavily eroded due to the high waves generated by the cyclone. Although effects were lesser in Vanuatu, the country's northernmost islands experienced heavy flooding and beaches destroyed by high waves. After this usage of the name Zoe, the name was retired.

Meteorological history

The origins of Severe Tropical Cyclone Zoe can be traced back to a convective cloud cluster, that had developed by December 22, within the South Pacific Convergence Zone to the north of the Samoan Islands. The system subsequently emerged out of the South Pacific Convergence Zone and was classified as Tropical Depression 04F, while it was located to the east of Funafuti in Tuvalu. Over the next couple of days the system was steered towards the west-southwest, under the influence of a mid-level subtropical ridge of high pressure.

After the depression had crossed the International Dateline early on December 25, atmospheric convection surrounding 04F increased and the system became better organized. At this time vertical wind shear over the system rapidly decreased, while the systems outflow significantly improved. As a result, the United States Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert on the system, before they initiated advisories on the system and designated it as Tropical Cyclone 06P. Later that day at 21:00 UTC (08:00 December 26 SIT) the FMS reported that the depression had become a Category 1 tropical cyclone, on the Australian tropical cyclone intensity scale and named it Zoe. At this time the system was located about 220 km (135 mi) to the northwest of the Fijian Dependency; Rotuma and moving westwards at about 18 km/h (11 mph).

After being named, Zoe intensified very rapidly in very favorable conditions and became a Category 3 severe tropical cyclone by 12:00 UTC (23:00 SIT) on December 26. Zoe's eye subsequently became obvious on both visible and infrared satellite imagery, while the system continued to intensify and became a Category 5 severe tropical cyclone during December 27. During December 27, the JTWC reported that Zoe had become equivalent to a category 5 hurricane on the Saffir-Simpson hurricane wind scale as it peaked with 1-minute windspeeds of 285 km/h (180 mph) and passed about 50 km (30 mi) to the southeast of the Solomon Island: Anuta. Zoe subsequently turned towards the southwest and passed in between the Solomon Islands of Anuta and Fataka, as the subtropical ridge weakened in response to an upper level trough of low pressure over the Tasman Sea. Early on December 28, the FMS estimated that the system had peaked as a Category 5 severe tropical cyclone, with 10-minute sustained wind speeds of 240 km/h (150 mph) and a minimum pressure of 890 hPa (26.28 inHg). By this time the steering flow over the cyclone had become weak and variable, as the system passed within 30 km (20 mi) of the island of Tikopia. As a result, Zoe virtually stalled and performed a small clockwise cyclonic loop, within the vicinity of Tikopia, however, the eye of the system did not pass over the island.

During December 29, after the system had stalled, Zoe started to move towards the southeast in response to the strengthening steering flow, provided by an upper level trough of low pressure and a baroclinic system near New Caledonia. Over the next couple of days the system rapidly weakened under the influence of: strengthening vertical wind shear, dry air and cooler sea surface temperatures. During December 31, as the system continued its southeastwards movement, it passed about 390 km (240 mi) to the southwest of Nadi, Fiji as a Category 2 tropical cyclone. By this time the system was transitioning into an extra tropical cyclone, while deep convection surrounding the system had significantly diminished. As a result of further weakening, the JTWC issued their final warning on Zoe during January 1, 2003, while the FMS reported that Zoe had weakened into a tropical depression. The system was subsequently recurved and started to move towards the southwest during January 2, before it was declared extratropical as it interacted with an extratropical low which was located over the Tasman Sea. Zoe was subsequently last noted by the FMS during January 4, while it was located about 367 km (230 mi) to the southeast of Noumea, New Caledonia.

Intensity

At its peak intensity Zoe was estimated by the FMS to be a Category 5 severe tropical cyclone, with 10-minute sustained wind speeds of 240 km/h (150 mph) and a minimum pressure of 890 hPa (26.28 inHg). Zoe was the most intense tropical cyclone in the Southern Hemisphere until a 2017 reanalysis of Cyclone Winston estimated a minimum pressure of 884 hPa (26.10 inHg), surpassing Zoe. The United States Joint Typhoon Warning Center reported that the system had peaked with 1-minute sustained wind speeds of 285 km/h (180 mph) and a minimum pressure of 879 hPa (25.96 inHg). Both of these intensity estimates were based on a subjective application of the Dvorak technique, as there were no direct observations of the system's intensity.

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